MACKENZIE ISLAND PROPERTY DOME TOWNSHIP ......Attention: Don Hoy Tel: (807) 346-0777 By: JVXLtd. 60...

1742 OA LOGISTICAL AND INTERPRETIVE REPORT

ON

SPECTRAL IP AND RESISTIVITY

SURVEYS

CONDUCTED ON THE

MACKENZIE ISLAND PROPERTY

DOME TOWNSHIP

NORTHWESTERN ONTARIO

RED LAKE MINING DIV.

JVXLtd.

52N04SW0144 2.17420 DOME 010

A LOGISTICAL AND INTERPRETIVE REPORT

ON

SPECTRAL IP AND RESISTIVITY SURVEYS

CONDUCTED ON THE

MCKENZIE ISLAND PROJECTDOME TOWNSHIP

NORTHWESTERN ONTARIO

For: Freewest Resources Canada Inc.800 Rene Levesque Blvd. W Ste. 1525Montreal, QuebecH3B 1X9Attention: Mac WatsonTel: (514) 878-3551Fax:(514)878-4427

Freewest Resources Canada Inc.855 Field Street Thunder Bay, Ontario P7B 6B6Attention: Don Hoy Tel: (807) 346-0777

By: JVXLtd.60 West Wilmot St, Unit #22 Richmond Hill, Ontario L4B 1M6

Contact: Blaine Webster Tel: (905) 731-0972 Fax:(905)731-9312 JVX Ref: 9602 February 17, 1996

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TABLE OF CONTENTS

1 INTRODUCTION..................................................^

1.1 GENERAL....................................................................................................................................................61.2 PURPOSE.....................................................................................................................................................6

2 DATA ACQUISITION .......................................................................................................................................7

2.1 SURVEY SPECIFICATIONS ......................................................................................................................72.2 GRID SPECIFICATIONS ............................................................................................................................72.3 PRODUCTION SUMMARY........................................................................................................................72.4 PERSONNEL................................................................................................................................................92.5 FIELD INSTRUMENTATION ..........................................................................................^.......Zl..^^^

3 DATA PROCESSING............................................^

3.1 IP AND RESISTIVITY .............................................................................................................................. 10

4 INTERPRETATION METHODOLOGY......................................................................................................12

4.1 IP AND RESISTIVITY ..............................................................................................................................12

5 DISCUSSION OF RESULTS...........................................................................................................................14

5.1 ANOMALY DESCRIPTIONS ...................................................................................................................14

6RECOMMENDATIONS..................................................................................................................................17

52N04SW01442.17420DOME 0 1 OC

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FIGURES

Figure l: Location Map

Figure 2: Grid Map

TABLES

Table l: Specifications for the IP/Resistivity Survey

Table 2: Summary for IP/Resistivity Survey (a^25 m )

APPENDICES

Appendix A: Background to the Geophysical Methods

Appendix B: Plates

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PLATESGRID l

Black and White Line Plots:

Plate l: Chargeability Contour Plan Map (11=2), Scale l :2400

Plate 2: Resistivity Contour Plan Map (11=2), Scale l :2400

Plate 3: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 1200E to L O, Scale 1:2400

Plate 3a: Stacked Spectral IP Pseudosections; MIP and Tau L 1200EtoLO, Scale 1:2400

Plate 4: Stacked IP Pseudosections; Chargeability and Apparent Resistivity; L 300W to L 1500W, Scale 1:2400

Plate 4a: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 300W to L 1500W, Scale 1:2400

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GRID 2

Black and White Line Plots:

Plate l: Chargeability Contour Plan Map (^1=2), Scale l :2400

Plate 2: Resistivity Contour Plan Map (11=2), Scale l :2400

Plate 3: Stacked Spectral IP Pseudosections; MIP and Tau L 2400N 8c L 2100N, Scale 1:2400

Plate 4: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 1800n to L 1200N, Scale 1:2400

Plate 4a: Stacked Spectral IP Pseudosections; MIP and Tau L ISOONtoL 1200NO, Scale 1:2400

Plate 5: Stacked IP Pseudosections; Chargeability and Apparent Resistivity; L 900N to L 300N, Scale 1:2400

Plate 5a: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 900N to L 300N, Scale 1:2400

Plate 6: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L O to L 900S, Scale 1:2400

Plate 6a: Stacked Spectral IP Pseudosections; MIP and Tau L O to L 900S, Scale l :2400

Plate 7: Stacked Spectral IP Pseudosections; Chargeability and Apparent Resistivity; L 1200S to L 1800S, Scale 1:2400

Plate 7a: Stacked Spectral IP Pseudosections; MIP and Tau L 1200S to L 1800S, Scale 1:2400

GRID l Si GRID 2

Plate 8: Compilation Map, Scale l :2400

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l INTRODUCTION

1.1 GENERAL

JVX Ltd. conducted time-domain spectral induced polarization (IP) and resistivity surveys from January 15 to February l, 1996, on behalf of Freewest Resources Canada Inc. The surveys were done on McKenzie Island, on the McQuaig Red Lake Gold Mine Property and joining properties in Dome Township, Northwestern Ontario (N.T.S. 52 N/4). The area is accessible by winter road from Balmertown., Ontario.

1.2 PURPOSE

The purpose of this survey was to map the sulphide iron formation and to relate known gold mineralization to various structures on the property. Two possible mineralization trends exist; one parallel to lithologic strike and one crosscutting geologic strike. Two grids were surveyed one crosscutting geologic strike and one crosscutting a mineralization trend from the Campbell and Dickenson Mines.

The data from the grid crosscutting lithothology gave better line to line correlation of the IP anomaly zone. The spectral data located several targets some of which were drilled previously with gold intersected. ( No. l Vein)

-- SURVEY AREA

LOCATION MAP

FREEWEST RESOURCES INC.MCKENZIE ISLAND PROPERTY

Red Lake Area, Ontario N.T.S. 52 N/4

GROUND GEOPHYSICAL SURVEY

Surveyed by ]VX Ltd. February 1996

Scale : 1 : 2,500,000

Figure l

Lake

L a k

McKenzie Island.**0

Lake

BASE LINE O GRID 2

GRID MAP

FREEWEST RESOURCES INC. MCKENZIE ISLAND PROPERTY

Red Lake Area, Ontario N.T.S. 52 N/4

0 GROUND GEOPHYSICAL SURVEY

Surveyed by JVX Ltd. February 1996

Figure 2

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2 DATA ACQUISITION

2.1 SURVEY SPECIFICATIONS

Table 1: Specifications for the IP/Resistivity Survey

I.P.7Resi5tivity

Transmitter

Receiver

Array Type

Transmit Cycle Time

Receive Cycle Time

Number of Potential Electrode Pairs

Electrode Spacing (a spacing)

Number of Lines Surveyed

Survey Coverage

Scintrex TSQ3/3.0 kW

ScintrexIPR-12

Pole-Dipole

2 sec

2 sec

8

100 feet

Grid 1 - 9 lines

Grid 2- 15 lines

60 600 ft (18 483m)

2.2 GRID SPECIFICATIONS

The survey grid, located on McKenzie Island in Dome Township, Balmertown area , Red Lake District of Northwestern Ontario, is shown in Figure 2.

2.3 PRODUCTION SUMMARY

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Total IP coverage was 60600ft (18 483metres). The following table lists the survey coverage in detail:

Line

1200 E600 E300 E

0 E-300 W-600 W-900 W

-1200 W-1500 W

Line

2400 N2100 N1800 N1500 N1200 N900 N600 NSOONON

-300 S-600 S-900 S

-1200 S-1500 S-1800 S

- J:.,; 1:.::-:^ '-îiVi;-;^^"^ -

Station from

1300 S1500 S1600 S1700 S1800 S1900 S1900 S1900 S1900 S

;-:-.-:: ::j?-. "-** 1 1.)? " ' .' ' ; ??"*; * ': '- '

Station from

100 E100 E100 E400 E700 E800 E1000 E1300 E1600 E1900 E1600 E1300 E600 E600 E600 E

TOTAL ALI

iCftiiJok S^: - .

to

400 S3000 N2800 N2400 N2000 N1900 N800 N800 N700 N

SubtotalISIiJlr '7

to1200 W1200 W800 W1400 W1600 W1600 W1200 W1200 W900 W1500 W1800 W1800 W1400 W1000 W1000 W

Subtotal, GRIDS

- ^X'l'-'^mDistance

(ft)

100045004400410038003800270027002600

29600-:; ' " •'/fff'^-f^,fjgf^

Distance (ft)

13001300900180023002400220025002500340034003100200016001600

3100060600

8

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2.4 PERSONNEL

Fred Moher (Geophysical Party Chief):Mr. Moher operated the Scintrex IPR-12 receiver and was responsible for data quality and theday-to-day operation and direction of the survey.

Four field assistants were also engaged by JVX.

Alexandra Savic (Geophysicist):Ms. Savic processed the data, prepared the plots, and is responsible for the data storage.

Dagmar Piska (Draftsperson):Ms. Piska carried out all manual drafting, and assembled and bound the report.

Slaine Webster (President, JVX Ltd.):Mr. Webster provided overall supervision of the survey, interpreted the data, and wrote thereport.

2.5 FIELD INSTRUMENTATION

JVX supplied the geophysical instruments described below. Additional information about the geophysical methods may be found in Appendix A.

2.5.11.P. TransmitterThe Scintrex TSQ3/3.0 kW Time Domain Transmitter powered by a ten-horsepower motor generator was used. The transmitter generates square wave current output with a period of 4, 8, or 16 seconds. A digital multimeter in series with the transmitter is used to measure the magnitude of the current output.

2.5.2 I. P. ReceiverThe Scintrex IPR-12 Time Domain Receiver was used. This unit samples the voltage decay curve as measured by the potential electrodes at ten points in time. Readings are repeated until they converge to within a tolerance level, and the data are stored in solid-state memory.

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3 DATA PROCESSING

After being transferred to a field computer at the end of each survey day, the data were examined, corrected, and organized by the instrument operator. The results were plotted on the following printers:

* STAR NX-80 colour dot-matrix printer ' EPSON FX-80 dot-matrix printer

These plots were used to monitor progress and data quality, and to make an initial interpretation. Thus survey parameters and design were altered when necessary.

The data were sent by courier to the head office of JVX in Richmond Hill, Ontario. They were processed and results were plotted on the following printers as was necessary:

* HEWLETT PACKARD DESIGNJET 750C 36 inch colour plotter* NICOLET ZETA 36 inch pen plotter* TEKTRONIX COLORQUICK ink jet printer" FUJITSU DL2400 colour dot-matrix printer* TEXAS INSTRUMENTS MicroLaser Pro 600 Laser printer

The processing procedure is outlined below.

3.1 IP AND RESISTIVITY

Steps l and 2 were performed both in the field and in the head office. Steps 3 and 4 were performed at the head office.

1) The GEOPAK IPSECT Package was used to generate colour pseudosections of chargeability and resistivity data.

2) JVX software was also used to perform spectral analysis of the time-domain data. This step was crucial to maximizing the information that can be obtained from IP data. This software analyses the shape of the IP decay curve, giving information about:

(a) the grain size (indicated by the parameter T),(b) the uniformity of the grain size (indicated by c}, and(c) the magnitude of the chargeable source (indicated by M-IP).

(Please see Appendix A for more information about spectral analysis.)

JVX

3) The pseudosections from 2 above were aligned in AUTOCAD, then plotted. Since chargeability values are quite low over this grid, none are presented in this report.

4) Contoured plan maps of both chargeability and resistivity data from one dipole were produced using JVX in-house software and the GEOPAK or GEOSOFT Line Processing Package. Additional drafting on these maps was done manually or through AUTOCAD.

11

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4 INTERPRETATION METHODOLOGY

JVX uses its many years of experience in geophysical interpretation to extract the most accurate information from the data. The procedures involved are simplified for the sake of clarity. The SPECTRAL data was extensively used to further define the grain size (fine or coarse- grained). The high chargeability amplitude associated with the iron formation made it difficult to select drill targets on chargeability alone therefore IP anomalies with fine-grained SPECTRAL responses were given a high priority for drilling.

4.1 IP AND RESISTIVITY

The IP and resistivity data are interpreted using the following procedure:

1) Chargeability anomalies are picked on the pseudosections and classified using the following scheme as a guide:

Very Strong (^ 30 mV/V) and well defined

Strong (20 to 30 mV/V) and well defined

Moderate ( 10 to 20 mV/V) and well defined

Weak (5 to 10 mV/V) and well defined

Very Weak (3 to 5 mV/V) and poorly defined

x x x x Extremely Weak ^3 mV/V) and very poorly defined

The peak of the anomaly provides a qualitative indication of the depth to the top of the anomalous source and the location of the centre of the body. Where possible, the location and dipole number of the peak are written beside the anomaly bar.

2) The SPECTRAL characteristics of the anomalies are examined. The peak value of M- IP is noted, and T is classified according to the following scheme:

L Long (? 3 0.0 sec)

M Medium ( l.0 to 30.0 sec)

S Short ^ l .0 sec)

12

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3) Resistivity anomalies are picked on the pseudosections and classified using the

following scheme as a guide:

no symbol VH(n) Very High ^ 30, 000 Qm) highly silicified

no symbol H(n) High p 1 0 000 Qm) probably silicified

no symbol WH(n) Weak High ^ 1 0 000 Qm) - relative increase comparedto surrounding material

SL(n) Strong Low — strong decrease in resistivity

- - - ML(n) Medium Low — medium decrease in resistivity

' ' " " WL(n) Weak Low — weak resistivity decrease relative to surroundingmaterial,

where n is the dipole number at which the anomaly peak is located.

4) The anomalies from steps l to 3 are marked on the Compilation Map.

5) Resistivity anomalies on the Compilation Map are joined into conductive and resistive

zones.

6) Zones of high chargeability are interpreted based on resistivity and geometric

information.

7^1 The chargeability anomalies are further prioritized employing the^SPECTRAL } parameters paying particular attention to the relative amplitude of the Mff response

and the length of the time constant.

8) The IP and Resistivity data is reviewed on the compilation map with ancillary

geologic and geochemical data.

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5 DISCUSSION OF RESULTS

The interpretation of the geophysical data was compiled onto a single map, and is summarized in the sections following. This Compilation Map and all data plots are included in Appendix B.

Three main IP chargeability zones have been mapped out on Grid 2 whose wing lines cross the stratigraphy. The anomalies are correlatable from line to line therefore it is assumed Grid 2 is the best map to use for stratigraphic correlation. The chargeability anomalies, resistivity responses drill holes and gold showings are identified on the Compilation Map (Plate 8).

5.1 ANOMALY DESCRIPTIONS

S.la ZONE IP -1 (Line 900S/800E to Line 1800N/200W)

IP zone IP-1 is a moderate to very strong, north/south trending, chargeability zone located on the eastern part of the grid. This zone strikes to the north extending between lines 900S and l SOON traversing a wide zone of high resistivities on the eastern part of the grid. The trend of IP-1 is parallel with the direction that drill holes l, 2, 5, 9, 10, l land 12 were drilled. The SPECTRAL data shows that even though the volume of sulphide is high the mineralization is fine-grained. In our experience this is a very good area to test for gold. Normally the alteration zone associated with a an auriferous sulphide body gives a short time constant. The section of IP-1 on line 300N which crosses with vein number l has a short time constant thereby indicating that the auriferous sulphide mineralization has a short time constant response and is therefore fine-grained. The combination of very high MIP (greater than 1,000 mV/V) with a short time constant is a very good gold indicator.

RECOMMENDATIONS:

Five targets have been selected on IP zone IP-1.

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TARGET l (Tla&Tlb) ( 300E/300N) High Priority

On grid l at 300E/300N the SPECTRAL response on a line surveyed parallel to geologic strike had a very high MIP response (zero time chargeability) with mixed time constants. Tib occurs 100 feet north of gold showing number 5 and 100ft. south of vein number l indicating the high MIP and short time constant is important in selecting drill targets.

The anomaly on line 300N/100E Grid 2 has a strong chargeability response with high resistivities (10-20,000 ohm-m) indicating a silicified environment. The SPECTRAL parameter Tau indicates that the source is fine-grained. Tla/Tlb occur near the projected western extension of the number l vein which makes this a high priority target. The anomaly should be drilled on line 300N. Geology should be used to further refine this target.

Tla and Tib are high priority drill targets.

TARGET T-3 (1200N/100E) Medium Priority

T-3 is a strong chargeability anomaly with low time constants correlating with a narrow resistivity high. The short tune constants and resistivity high indicate a fine-grained silicified source.

T-3 is a medium priority drill target.

TARGET T-4 (300S/300S) Very High Priority

T-4 is a very strong chargeability anomaly which is associated with a slight resistivity increase and moderate-to-high SPECTRAL MIP indicating a very high volume percent of fine-grained sulphides.

T-4 is a very high priority gold target. The anomaly should be drilled on line 300S. Geology should be reviewed to further prioritize the targets.

TARGET T-5 (1800N/200W) Medium Priority

T-5 is a very strong shallow chargeability response located on the east flank of a resistivity low near gold showing number l.

T-5 should be evaluated geologically and geochemically

Target T-5 could be moved to either line l SOON or l SOON.

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Target T-6 (600S/900E) Medium Priority

T-6 is a very strong chargeability anomaly with a moderate SPECTRAL MIP response and an associated long time constant (TAU). A narrow weak resistivity high (3,000 ohm-m) occurs on its west flank.

Gold showing #4 is located 400ft. to the east and may have a relationship with T-6. Drill holes 7 and 8 may partially explain T-6 and should therefore be evaluated for sulphides and alteration.

5.2 IP Zone-2 (Line 1500S/100W to Line 900S/500W)

IP Zone 2 is a moderate to strong chargeability anomaly zone associated with a resistivity high located on the southwest part of the grid on a small island. The short time constant indicates the source to be fine grained; this together with the high associated resistivity suggests that the sulphide source may be silicified.

Recommendation:

TARGET 2 (1200s7300W) Very High Priority

The SPECTRAL MIP is moderately high but the SPECTRAL TAU indicates a fine-grained source. Strong chargeabilities occur on the western contact of a very highly resistive body. The anomaly is duplicated on line 9W/4S.

The geology associated with IP Zone 2 is quartz porphyry, andesite agglomerate, and iron formation, an excellent gold environment.

5.3EPZone-3a (Line 600W/600S to Line 00/400S) IP Zone -3b (Line 900W/500S to Line 1500W/600S)

IP Zones 3a and 3b are strong chargeability anomaly zones associated with a resistivity high located on the southwestern part of the grid and situated on the northeastern part of a small island.

The associated geology should be reviewed and further evaluation made after target T-2 is drilled.

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6 RECOMMENDATIONS

All target areas should be visually inspected and sampled. The present drill program will test the defined target areas. Prior to drilling, we recommend IP modelling of relevant anomalies.

The core should be logged with special attention paid to fine grained and coarse grained sulphides and their association with silicification/alteration and gold mineralization so that the spectral data can be correlated to grain size. Explanations of targets should be given to JVX as a further guide in its spectral interpretation.

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If there are any questions with regard to the conducting of the survey or the interpretation of the data, please call the undersigned at JVX Ltd.

Respectfully submitted,

JVX Ltd.

Blaine Webster, B.Sc. President

18

APPENDIX A

Background

to the

Geophysical Methods

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INDUCED POLARIZATION AND RESISTIVITY

l THE IP EFFECT

The induced polarization (IP) phenomenon is primarily caused by:

1) electrical polarization at the boundary between the rock or soil and the pore fluids, and

2) electrical polarization at the boundary between metallic minerals (particularly sulphides) within pores and the pore fluids.

This polarization occurs when a current is applied across these boundaries. Its magnitude can be measured in two ways:

1) in the frequency domain (also known as phase IP), in which the applied current is sinusoidal, or

2) in the time domain, in which the applied current is a modified square wave.

JVX conducts IP surveys in the time domain because spectral analysis, a powerful interpretive tool, can only be performed in the time domain.

Generally, the current is transmitted as a modified square wave with a period of eight seconds (two seconds positive, two seconds off, two seconds negative, two seconds off). The voltage measured in the ground will have the form shown in figure IP-1. The IP effect is manifested as a roughly exponential voltage decay after the current is turned off, similar to the relaxation effect of a discharging capacitor. The IP receiver samples this voltage decay curve at a number of points.

The SCINTREXIPR-11 receiver repeats and averages the following measurements until they converge:

Vp The primary voltage (the steady-state amplitude of the voltage while the current is being transmitted).

IP-1

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SP The self-potential (the steady state voltage when no current is being transmitted).

mO to m9 The chargeabilities (measures of the IP effect at different times along the decay voltage curve Vs(t) ).

Each chargeability value (mO to m9) is the ratio of the average secondary voltage over a time window to the primary voltage. Mathematically, this is given by:

f"m = 1 000 l Vs(t) dt

Vp(Vt,) J t,

wherem = chargeability (in mV/V)

Vs(t) = secondary voltage (i.e. the voltage decay) Vp = primary voltage t, = beginning of time window t2 = end of time window

The IPR-11 uses the ten time windows, also known as time slices, listed in table IP-1 and shown in figure IP-2. Unless otherwise stated, the term chargeability refers to the eighth time window (m7).

IP-2

Vp

T3 do

SP

Vs(t)

Figure IP-1 : The I.P. Waveform

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SLICE

mO

ml

m2

m3

m4

m5

m6

m8

m9

DURATION (msec)

30

30

30

30

180

180

180

360

360

FROM (msec)

30

60

90

120

150

330

510

1050

1410

TO (msec)

60

90

120

150

330

510

690

1410

1770

MIDPOINT (msec)

45

75

105

135

240

420

600

1230

1590

Table IP-1 : Time slices recorded by the IPR-11 receiver

Nominal total receive time: 0.2.1.2,4 sec.

y.

i; ;i s.

0-3 4 5

11111 6t 6t A Delay

M

6t

7

12t

M8

12t

M,'9

12t Window Width

IPR-11 TransienlWindows

Figure IP-2 : IP effect decay curve with IPR-11 time slices

IP-4

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2 SPECTRAL ANALYSIS

With the ability to sample the decay curve at a number of points, the shape of the decay curve can be analysed. This gives important information about the characteristics of the source.

Spectral analysis utilises the Cole-Cole model of the IP effect (Pelton et al., 1978). This model uses the following four parameters (described in Johnson, 1984) to calculate a theoretical IP decay curve:

pa Resistivity (Qm)This quantity is described in detail later in this appendix.

M-IP Chargeability Amplitude (mV/V)This quantity is related to the volume percent of the chargeable source, although there is no simple quantitative relationship.

T Time Constant (seconds)The time constant is related to the grain size of the source. A short time constant (0.01 to 0.3 s) indicates a fine-grained source. A long time constant (30 to 100 s) indicates a coarse-grained, interconnected, or massive source.

c Exponent (dimensionless)A high value (e.g. 0.5) indicates that the grain size is uniform. A low value (e.g. 0.1) indicates that there is a mixture of grain sizes.

Conventional chargeability is a combination of these spectral parameters. A change in any one parameter will produce a change in the apparent chargeability. In the absence of spectral analysis, such changes are always ascribed to a change in the volume percent of the chargeable source, even though the cause may be a shiftfromjme-grained to coarse- grained material.

JVX has developed a software package called SOFT n which determines the spectral parameters by comparing the measured decay curve with a library of model curves. The quality of the fit is given as a root-mean-square difference (expressed as a percentage). A low value (e.g. l 07o) indicates high quality data of medium to high amplitude. A high value (e.g. greater than 10 07o) indicates poor quality or low amplitude data. If the fit is greater than 5 9-6, the spectral parameters are considered to be of poor quality, and therefore are usually discarded.

IP-5

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3 ARRAY CONFIGURATION

As mentioned above, a current must be flowing through the ground in order for the IP effect to occur. This current is applied using two electrodes, which are called CI and C2, and the voltage decay is measured using two potential electrodes, PI and P2. The distance separating PI and P2 is known as the a-spacing, or o, and generally remains constant during the survey.

The three most common electrode array configurations are:

1) GradientCI and C2 are located at an "infinite" distance (i.e. very far) from the grid, with one on each side. The potential electrodes move throughout the grid.

2) Dipole-DipoleC l and C2 are separated by a distance of o, and move along with the potential electrodes.

3) Pole-DipoleC2 is located at "infinity". CI moves along with the potential electrodes throughout the grid.

The gradient array allows for fast reconnaissance surveys. However, no depth information is obtained (described below), and the resolution is much lower because all of the ground between CI and C2 is energised. Furthermore, the current will be channelled through conductive zones, which could result in inaccurate chargeability and resistivity values. Thus, great care must be used when using a gradient array.

In JVX1 experience, the pole-dipole array is superior to the dipole-dipole array. Since C2 is located at an infinite distance, a greater volume of ground is energised. This results in better depth penetration (i.e. higher quality data), and is particularly important in the presence of thick and/or conductive overburden. However, the pole-dipole array does not have the disadvantages of the gradient array. Since CI is located near the potential electrodes, depth information is obtained (see below), and resolution is high.

4 A-SPACING AND NUMBER OF DIPOLES

The resolution of the data depends on o, the electrode spacing. The smaller a is, the greater the resolution. However, the depth of penetration is also smaller. A larger a results in greater depth, but less resolution. Thus, both factors must be considered when selecting the electrode spacing.

The standard pole-dipole array is shown in figure IP-2. Seven potential electrodes are used to measure the voltage simultaneously across six electrode pairs (P1-P2, P2-P3, P3-

IP-6

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P4, etc.). Each pair is labelled using an integer, n, where na is the distance between the first potential electrode and the nearest current electrode.

The depth of investigation is greater when the potential electrode pair is farther from the current electrode (i.e. larger n). However, a greater separation distance also results in greater signal attenuation, limiting the number of dipoles which could be used effectively.

5 RESISTIVITY

The DC apparent resistivity (pa) is a measure of the bulk electrical resistivity of the subsurface. Electricity flows primarily through the groundwater within fractures and pore spaces. Therefore, fault zones can be detected as low resistivity zones. However, sulphide minerals, some oxides, and graphite are also good conductors and so produce low resistivity zones. The current flow is electronic in these minerals rather than electrolytic as it is in groundwater. Sometimes, the geometry of the low resistivity zone can distinguish between a fault zone and a mineral source. In other cases, additional geological information is needed. Silicates, the most common rock forming minerals, are very poor conductors of electricity, producing high resistivity zones.

The resistivity is measured simultaneously with the IP data. For a homogeneous and isotropic subsurface, it is given by the following formula:

wherepa = apparent resistivity (Qm)

Vp = primary voltage (measured while current is on) (mV) k :: k-factor (m)

The k-factor is an array-dependant component. For a pole-dipole array, it is given by:

k s 27cn(n*l)a

wheren = dipole multiple (dimensionless) a = electrode separation (m)

Although the assumption of a homogeneous and isotropic earth is unrealistic, the calculated value of pa can be used qualitatively to map changes in rock type (even to identify the rock type in some cases), and to map low resistivity fault zones.

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References

Johnson, I.M. Spectral I.P. Parameters as Determined through Time Domain Measurements, pp. 1993-2003 Geophysics 49, 1984

Johnson, I.M., B. Webster, R. Mathews, and S. McMullan Time Domain Spectral IP Results from Three Gold Deposits in Northern Saskatchewan, The Canadian Mining and Metallurgical Bulletin, Feb. 1989

Pelton, W.H., S.H. Ward, P.G. Hallof, W.P. Sill, P.H.Nelson Mineral Discrimination and Removal of Inductive Coupling with Multifrequency IP. pp. 588-609, Geophysics 43, 1978

IP-8

APPENDIX B

Plates

GRID 1

l T96925 i

1209693 '^r^

FREEWEST RESOURCES CANADAFigure!

Claim Location SketchMcCuaig Red Lake Property

McKenzie Island, Dome TownshipRed Lake Mines 8i Minerals Division

RECEIVED

JUN 20 1997

MINING LANDS BRANCH

GRID 2

GRID 1 SL G RID 2

Compilation Map

D OhtariO 1̂ ******* Declaration of Assessment Work A and Mines Performed on Mining Land

Mining Act, Subsection 65(2) and 66(3), R.S.O. 1990

Transaction Number (ellice use)

Assessment Files Research Imaging

Personal information colled Mining Act, the Information i Questions about this colle 933 Ramsey Lake Road, Si

of the Mining Act. Under section 8 of the nd correspond with the mining land holder, ern Development and Mines, 6th Floor,

52N04SW0144 2.17420 DOME 900

Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. - Please type or print in ink.

1 . Recorded holder(s) (Attach a list if necessary)

AyName Client Number

Address Telephone Number

Fax Number

NameEiUrfgl

Client Number

Address Telephone Number

Fax Numbe

2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration.

Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

Physical: drilling, stripping, trenching and associated assays [ l Rehabilitation

Work Type It -Z /9^ kil*e4r6 k ^f^*t Jw&a*1- fyt6frt*4n*

j^^/5-fv/ly 5uMfe ( io .̂ )

Dates Work . f . T Performed From * ' *ai '

Day Month Year n 7 If DayGlobal Positioning System Data (if available) Township/Area

GrJ*

Month Year

M or G-Plan NumberG-T7M-8

Office Use

Commodity

Total S Value of f̂ f-\ ' 7 ^^ Work Claimed ^(. i ^T^f -

NTS Reference f) 3/1 7 xi (̂-56t

Mining Division A J^ -/Ô

Resident Geologist /} s x District A^td fa*~#-i^

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Person or companies who prepared the technical report (Attach a list if necessary)Name .

W U}^ UJi/nW 5{fV^, i/nJ^ ^22, I?idUwi^ f^l(, rf*(Wrr ^ /'ft

Name

Address

Name

Address

Tele)

Fax h

0Tele;

Fax h

hone Number 6*ti 3-3 f-d If l*-

jCtiC^-r^ L. i "w L li

tone Nurnbar, ^ JUNfi f

2 0 1997umber

MINING LANDS BRANCHTelephone Number

Fax Number

4. Certification by Recorded Holder or Agent

l, , do hereby certify that l have personal knowledge of the facts set(Print Name)

forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.

5. Work to be. recorded and distributed. the* mining land where work was performed, must accompany this form.

Work can only be assigned to claims that are contiguous (adjoining) at the time work was performed. A map showing the contiguous link

L{) c{7 36 - O O /~JOMining Claim Number. Or K work wu dona on other eligible mining land, show In this column the location number indicated on the claim map.

eg

eg

eg

1

2

3

- 4

5

6

7

8

9

10

11

12

13

14

15

TB 7827

1234567

1234568

/Z0W2-

l-KXbV

{ZOW}

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

?

Z

i.

t

Column Totals

Value of work performed on this claim or other mining land.

S26, 825

0

S 8, 892

Mfr

Wb

W,

2 fc. m

Value of work applied to this claim.

N/A

S24,000

S 4,000

' 1,2-00

f 2,0017

' ff*a

O 1til A *"JU * J*^^^^

:

t/, 000

Value of work assigned to other mining claims.

S24,000

0

0

742 (\

Bank. Value of work to be distributed at a future date.

S2,825

0

S4,892

TftVf

W

8 /It?

aa^b

l, , do hereby certify that the above work credits are eligible under(Print Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to

the claim where the work was done.

Signature of Recorded Holder or Agent Authorized in Writing Date

6. Instructions for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check ( s ) in the boxes below to show how

you wish to prioritize the deletion of credits:

D 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.

D 2. Credits are to be cut back starting with the claims listed last, working backwards; or

W 3. Credits are to be cut back equally over all claims listed in this declaration; or

D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

Note: If you have not indicated how your credits are to be deleted, c followed by option number*2 if necessary.

he Bank first,

For Office UseReceived Stamp

oÊGEIVEDRED LAKE MINING DIV.

JUN l fj J997

AM " W)

Deer fed Approved Date .

Date Approved '

Date Notilicatlon Sent

Total Value of Credit Approved

. h L

Ontario

Ministry otNorthern Developmentand Mines

Mmistere du Developpement du Nord et des mines

Statement of Costs for Assessment Credit

Etat des couts aux fins du credit d'evaluation

Mining Act/Loi sur les mines

Transaction No./N" de transaction

M- oo l "70

17420Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining claim(s). Questions about this collection should be directed to the Provincial Manager. Minings Lands, Ministry of Northern Development and Mines, 4th Floor, 159 Cedar Street. Sudbury. Ontario P3E 6A5, telephone (705) 670-7264.

Les renseignements personnels contenus dans la presente formule son! recueillis en vertu de la Lol sur les mines et servlront a tenir a jour un registre des concessions minieres. Adresser (oule quesiton sur la collece de ces renseignements au chef provincial des terrains miniers. minislere du Developpement du Nord et des Mines. 159, rue Cedar, 4* etage, Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.

1. Direct Costs/Couts directs

Type

Wages Salalres

Contractor's and Consultant's Fees Drolts de ('entrepreneur et de I'expert- consell

Supplies Used Fournltures utlllsees

Equipment Rental Location de mate'rlel

Description

Labour Main-d'oeuvre

Field Supervision Supervision sur le terrain

Type

J* 5c*wy

a&rfUVi^ M.4p

Type

""RECEIVHtU LAKE MININ

JUN l u |99?-.\

Amount Montan!

*1f,Wf

2,100

t

"i DIV.

PM

^S.SiWiyri^tt^&l8 Total descoUts directs

Totals Total global

'*Zw\

'is," j-'-îV-

fyW*

2. Indirect Costs/Couts indlrects* * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les couts indirects ne son! pas admissibles en tant que travaux d'evaluation.

Type

Transportation Transport

Food and Lodging Nourrlture et hebergementMobilization and Demobilization Mobilisation et demobilisation

Description

Type

- Amount Montant

Sub Total of Indirect Costs Total partlel des coOts Indlrects

Amount Allowable (not greater than 20tt of Direct Costs) Montant admissible (n'excedant pas 20 H des coOts directs)

Total Value of Assessment Credit Valeur totals du credit (Total of Direct and Allowable d'evaluationInrilrart rnalll (Total du COfHl dlrtetl

Totals Total global

tt Indirect* admissible*

Note: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment work all or part of the assessment work submitted.

Note : Le titulaire enregistre sera tenu de verifier les depenses demandees dans le present etat des couts dans les 30 jours suivant une demande a eel effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout ou une partie des travaux d'evaluation presentes.

Filing Discounts

1. Work filed within two years of completion is claimed at 100(Vb of the above Total Value of Assessment Credit.

2. Work filed three, four or five years after completion is claimed at 5Q0fa of the above Total Value of Assessment Credit. See calculations below:

Total Value of Assessment Credit Total Assessment Claimed

x 0.50

Certification Verifying Statement of Costs

l hereby certify:that the amounts shown are as accurate as possible and these costs were incurred while conducting assessment work on the lands shown on the accompanying Report of Work form.

that as(Recorderf'Holder, Agent, Position in Company)

to make this certification

Remises pour dep6t

1. Les travaux deposes dans les deux ans suivant leur achevement sont rembourses a 100 ^ de la valeur totale susmentionnee du credit d'evaluation.

2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement sont rembourses a 50 ah de la valeur totale du credit d'evaluation susmentionne. Voir les calculs ci-dessous.

Valeur totale du credit d'evaluati

Attestation de I'ttat de;

J'atteste par la presente :

n Evaluation totale demandee

xRC-C E 1 V E D

Co0t JUN 2 0 1997

MINING LANDS BRANCHque les montants indiques sont le plus exact possible et que ces depenses ont et6 engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-jolnt.

l am authorized Et qu'a litre de je suis autorisea mn? uo ——————.————————————————————— j~ ~— j ~ (titulaire enregistre, representant, posts occupe dans la compagnie)

a faire cette attestation.

Signature Dale

Ministry ofNorthern Developmentand Mines

August 26, 1997

EWAN STEWART DOWNIE 1529 RANKIN STREET THUNDER BAY, Ontario P7E-5Z2

Ministere du Developpement du Nord et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (888) 415-9846 Fax: (705) 670-5863

Dear Sir or Madam:

Subject: Transaction Number(s):

Submission Number: 2.17420

W9720.00170

StatusDeemed Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact Steve Beneteau by e-mail at [email protected] or by telephone at (705) 670-5855.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 11276

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .17420

Date Correspondence Sent: August 26, 1997 AssessorSteve Beneteau

Transaction First Claim Number NumberW9720.00170 1209692

Section:14 Geophysical IP

Township(s) l Area(s)DOME

StatusDeemed Approval

Approval Date

August 21, 1997

Correspondence to:Resident Geologist Red Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):Donald HoyTHUNDER BAY, ONTARIO

EWAN STEWART DOWNIE THUNDER BAY, Ontario

PERRY VERN ENGLISH RED LAKE, Ontario

Page: 1

Correspondence ID: 11276

AREAS W ITHDRAWN FROM DISPOSITION

MHO -M NING RIGHTS ONLY

S.R.O. SURf ACE RIGHTS ONLY

M.+ S. - I'/.iN'NGfAND SURFACE RIGHTS

Description Order No. Date Dijposition FiLa

SEC. 36 0.-M/88 30/06/88 MRO 188993

NOTE

SURFACE RIGHTS T RANSFERRED TO CANADA IN AREA

SHOWN THUS ; : AT RED LAKE AERODROIJE,

FILE 6 1894 R EF 141253 O C EO Dr LT?

LU

MCDONOUGH TOWNSHIP G 373241 M

M- - l M

3M- -

B o y

1197174J K796925

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j II44363J 1144364 i I OZ2726- - 4————— -L. - -

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LO l l l 7969O7

f 9 3L ~"~KRL ~|"KRL "T KRL~ "i"*-,

l 776201 l !*jx l 796919 | 796945 l 796939 l 796908 | 787586 | G) l II

-^(ff00907'

.^ KRL l KRLKRL! 79694 'h- --T-" - -T----T--

I fxr'U l p. n U. l i l776202 776200 ' 776210 796918 ,

' l ll.MM—— —— T— ——— — ~T~ —— "T~ l KRL

l KRL

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192 14 7 19215

^Jk^kN l 869619 in l

Qchenour— —l 869620

i ^8696ie— i __ __ —

m I/IKRLI S U 8 6961-

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KRL ' KRL •^"869383 ! "6995 l 83900

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1

—— - 4-—————.L.-.-

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904/501 l 904 f07. 1197550

II97D5Ilo*507 Uo4-5-06 90*5-05-

or( str'y ^t./?

______—— i, -- -I.——

9045-3-2. J ^4.5-33

Howey90.9*1

HEYSON TOWNSHIP G 3736

CD

m

o

COrrT)

CDOJ -JOJen

o oCM

LEGENDHIGHWAY AND HOTTF \o

' --t - "(..AuS

r (- A . .fiHH . t V f . 'Mr S

l i"j AM SHIPS. B A') t L !Nfc S. L K

IO1S MlMNC, (.1 A;MS PARLt.i i

UNS' 'K . F i F !'- i !"JL S il , . : .'^ -,

PA-^ r i -ri( M/NI.AM v

Ml 1 . 'M", i.:i AIMS f- Tt.

RA!|.'.-'-. A\[) HIGH I (If WA^t

i J T l; ' - j i N t S

\. '. (.. .^ \ MAL S T M(r AM

^ Li H ' V, OH F LOUOlNCi RIGHTS

Sl'H; 'ViSION OH COMPOSITE Pi AN

RESf R'. A V IONS

ORKjINAL SHOfU LIMF

MARSH OR MUSKtG

M IN f-S

TRAVF. RSI Mi;Nl JMtNT

DISPOSITION OF CROWN LANDS

SYMBOiTYPE OF DOCUMENT

PATFNT MJHfAC.f A MINING H K ,H l 1 .

SI. J (O At l RK,M T'. (iM N

MININi, MKjH T 1 , (JNI T

LtASt suHrAii s, MINING Hit,M ' .SI iRI At;f MM ,n i S i INI t

MiNiNt, UK,M -', ONI v

t ICF NCF Of (JfX.UPA T ION

ORtH R IN l.f )UN(.ll

R l SI H VAT ION

CANCf L l f O

SAND R. GRAVf t

NOTE M INlN' . Hi' .n I'., if/ c n H I f l '. l'A I l i* i l f j P H 11'i H T i U A . (,

1411 V l ', T J ( . l ^ ''i M l - . r N A l l' A ' i 'i M l H * l M l l 1 1) H t l (

L ANOS A f l H '. i ' 'l ") f u A' 1 l"'l M '.l M nil ' l

n uT

Of

SOOMplro,

i nonMvtrx

10 O 10 J O 1 0 40 Ml (,fl /o

soo o looa vooo 3000 lone

SCALL 1.20 OOO

FOREST ACTIVITY INFORMATIONTHIS TOWNSHIP/AREA FALLS WITHIN THE

RED LAKE CROWNAND MAY BE SUBJECT TO FORESTRY OPERATIONS. THE M.N R UNIT FORESTER FOR THIS AREA CAN BE CONTACTED AT:

P.O. BOX 5003RED LAKE, ONTARIO POV^MO(807) 727-2253

ft. 1742

THE INFORMATION T IAT APPEARS ON THIS MAP HAS BLEN COMPII ED FROM VARIOUS SOURC Ef,. AND ACCURACY IS NOT GUARANTEED. THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMAT-ON ON THE STATUS OF YHE LANDS SHOWN HEREON

TOWNSHIP

DOMEMMR ADMINISTRATIVE DISTRICT

RED LAKEMINING DIVISION

RED LAKELAND TITLES/ REGISTRY DIVISION

KENORA / PATRICIA

Ministry ofNaturalResources

Ministry ofNorthern Developmentand Mines

OntarioN ii m h *

SEPTEMBER I986

1600 W

1200 W

800 W

e

Strong

Strong

VVH(2) - Weak High Resistivity 1 H;1) - High Resistivity, 11=1 VHi2) - Vary High Resistivity, 0=2

Strong Resistivity Low

IP-1

vVeak l

M- l Pi TV Vi 517 . L lTimo Constant (Long,Medium or Short) —' |

Very Woak

Medium Medium Resistivity Low

Weak Resistivity Low

Very Woak Resistivity Low

DDH 1

Showing

^^

Chargcnbiiity Zono

Diamond Drill hole

Showing

CHARGEAE'LITV ANOMALY

RESISTIVITY ANOMALY

T-1" Exploration Target

VHP - Very High PriorityHP - High PriorityMP - Medium Priority

BASE LINE O GRID 2

2.l? 420

52N04SW0144 2.17420 DOME 210

FREEWEST RESOURCES INC.MCKENZIE ISLAND PROPERTY

RED LAKE AREA, ONTARIO_________N.T.S. 52 N/4_________

COMPILATION MAP

SURVEYED BY JVX LTD., FEBRUARY 1996

100 100 200 SOO

PLOTTED BYD.P.

FEE 1996SCALE I "s200' PLATE 8

JVX. ref. no. 9602

o o

2800 N

2700 N

2600 N

2500 N

2400 N

2300 N

2200 N

2100 N

2000 N

1900 N

1800 N

1700 N

1600 N

1500 N

1400 N

1300 N

1 200 N

1 100 N

1000 N

900 N

800 N

700 N

600 N

500 N

400 N

300 N

200 N

100 N

100 S

200 S

300 S

400 S

500 S

600 S

700 S

800 S

900 S

1000 S

1 100 S

1200 S

1300 S

1400 S

1500 S

1600 S

1700 S

o o CM o o 01o o10

o o o oto

o o(O

o oON

o o10

o o(N

o o en

o o(O

o oIO

UlooIO

Ulo o10

oCM CM

2800 N

2700 N

2600 N

2500 N

2400 N

2300 N

2200 N

2100 N

2000 N

1900N

1800 N

1700 N

1600 N

1500 N

1400 N

1300N

1200 N

1 100 N

1000 N

900 N

800 N

700 N

600 N

500 N

400 N

300 N

200 N

100 N

100 S

200 S

300 S

400 S

500 S

600 S

700 S

800 S

900 S

i s iooo s

1 100 S

1200 S

1300 S

420

FREEWEST RESOURCES CANADA INC.MCKENZIE ISLAND PROPERTY - GRID i

RED LAKE MINES and MINERALS DIVISION ______________N.T.S. 52 N/4

CHARGEABILITY CONTOURS (11=2)CONTOUR INTERVALS : l A 5 mV/V

TIME WINDOW 310-1050 ms

SURVEYED BY JVX LTD. USINGSCINTREX IPR-12 Rx ; IPC-7/2.5 kW Tx

WINTER 1996O 200 400 600

PLOTTED BYA.S.

FEB. 1996SCALE 1:2400 PLATE l

JVX ref. no. 9602

o oIf)

O O

2800 N

2700 N

2600 N

2500 N

2400 N

2300 N

2200 N

2100 N

2000 N

1900 N

1800 N

1700 N

1600 N

1 500 N

1400 N

1 300 N

1200 N

1 100 N

1000 N

900 N

300 N

700 N

600 N

500 N

400 N

300 N

200 N

1 00 N

100 S

200 S

300 S

400 S

500 S

600 S

700 S

800 S

900 5

1000 S

1 100 S

1200 S

1300 S

1400 S

1500 S

1600 5

1 700 S

o oO)

o o(O

o o

UJo oK)

g(O

o oCN

o oo oCN

o oO)

o o(O

o oO O ro

UJO O (O

2800 N

2700 N

2600 N

2500 N

2400 N

2300 N

2200 N

2100N

2000 N

1900N

1800 N

1700 N

1600N

1500 N

1400 N

1300N

1200 N

1 100 N

1 000 N

900 N

800 N

700 N

600 N

500 N

400 N

300 N

200 N

100 N

100 S

200 S

O CO (N

300 S

400 S

500 S

600 S

700 S

800 S

900 S

1000 S

1 100 S

1200 S

FREEWEST RESOURCES CANADA INC.

MCKENZIE ISLAND PROPERTY - GRID iRED LAKE MINES and MINERALS DIVISION

______ ______N.T.S. 52 N/4 ___________

RESISTIVITY CONTOURS (11=2)CONTOUR INTERVALS : 500 fc 2500 ohm m


WINTER 1996O 200 400 600

PLOTTED BYA.S.

FEB. 1996SCALE 1:2400 PLATE 2

JVX ret. no. 960Z

LINE : O E

INDUCED POLflRIZflTION SURVEY

POLE-DIPOLE RRRflY

DEPTH'VoiNT

N z l . 2. 3. 4. ... •fi" SPBCING : 100.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND, GRID-1

RED LflKE flREflDflTE : WINTER 1996 REF : 9602

SCflLE = l : 2400

JVX LTD.

15CJ05 | MODS | 13C|OS t 12CJOS | HOPS | l OOPS | 90pS | 80pS | 70pS , 60pS | SOpS | 40pS | 30pS | 20pS , IQpS | ON | IQpN | 20pN | 30pN t 40pN | SOpN | 60pN | 7PpN | 80pN L 90pN | IQÔN | ll^DN | 12(]ON [ 13(|ON | HC]ON 15(|ON | 160DN | 1TCJON | 18QON | 19QON | 20QON t 21DON

RESISTIVITYNil

N:2

N:3

Ni4

NiS

N:6

2. OK

nra.

.0 102.0 108.0 221.0 188

n:-j 19.0,361.O 27

RESISTIVITY265.0 .582J) 708-0 56.7-0,199.0 161.0 123-0 119.0 161.0 193-0-^s^s / /y ^--i ^— oo z-"*

DN

MX CHG.Nil

Ni2

N:3

N:4

N:5

N:6

7.7

10t]OS , 90pS | 60pS , 70pS | 60pS t 50pS 20pN t 30pN | 40pN | SQpN | 60pN | 70pN14C)OS | 13(|OS 2ops i tops 11CJON | 12(|ON t laqON | 14CJ N | 16C|ON | 17(]DN | IBtjON , 19C|ON | 20C)ON | 2KJ

r 31714.6 26-4

16.1 ^ 27.8

16.3 18.1/ 29.3 20

19. ff 30g) 22.2

MX CHO. Nil

N;2

Ni4

Ni6

LINE : 300 E


POLE-DIPOLE RRRflY

--o.DEPTH"*POINT

N r l . 2, 3. 4. •R" SPRUNG : 100.0 FEET



SCflLE = l: 2400JVX LTD.

15C]OS t 1 4^05 90pS | SOpS | 70pS , 60ps~~~~""~

40pS | 30pS t 20pS 20pN | 30pN 60pN | 70pN , BOpN , 90pN IBCj ON 2DQON 230^ | 24()ON , 250| ON , 260^~

RESISTIVITY

N:2

N:3

N:4

NiS

N:6

MX CHG.Nil

N:2

Ni3

N:4

N:5

N:6

60pN | 70pNS , 50pS | 40pS t 30pS | 20pS | IQpS N , 20pN | 30)N , 40pN 19CJON | 20C)ON 220| ON , 230| ON , 24C|DN , 250| ON | 26CJON | 270( ON

n-.'l't&'T-'tef'-) H-aj7 ~i*(s) .6, 24.8 27^2 -58.1 11.1 9

0 *28.

23.5 23.5

2.9 /24.1 21.3 23

4.7 22-0 21-7

RESISTIVITYNil

Ns2

Ni3

N)4

N:5

N:6

35.0

MX CHG. 12.t ,,,7 1.7 1.4 .8 .5 .1 .5 .6 .4 Nil

1.5 1.0 .3 .6 .8 .0 Ni2

.0 1-5 .9 .8 .9 -.1 Ni3

1.2 1.5 1.3 1.1 .1 Nt4

1-3 1.6 1.6 .6 N:5

Zv.0 1.5 2-0 .9 N:6

LINE : 600 E


POLE-DIPOLE flRRRY

DEPTH POIMT

N ; 1. 2. 3. 4. "fi" SPRCING : 100.0 FEET




14(]OS 12qOS lO IjOS t 9 0pS , 80pS t 7 0ps t SOpS | SOpS t 4 0pS L 30pS , 20pS--- — --- -""- - —— - ON , lOpN t 20pN , SOpN t 40pN | SOpN t 60pN t 70pN— — .-... 90N

RESISTIVITY

12(]ON 14(]ON | ISOCON 20QON | 220| ON , 23QON | 240| ON t 250| ON t 260) ON t 270| ON t 280( ON | 29QON

Nil

Nt2

Nt3

Ni4

NiS

N)6

5.4K

MX CHG.

N:2

Ni3

N)4

N)5

N:6

9.roo4.3K 8

10. IK *

Sops | 70pS pS | 40pS | 30ps , 20pS 20QN 8 3QpN , 40pN | SOpN ( 6QpN | 70pN | 80pN , 90p 230| ON t 240| ON | 250| ON | 260| ON | 270( ON , 28CJON t 290( ON

19.1 24.4 23.3 20.2 24

RESISTIVITY Nil

Ni2

Ni3

N:4

NiS

NiB

MX CHG. Nil

37.2

1.0 1.0 1.2 .9 .7 .4 -.1 -.4 -.4 -2.0

1.3 1-4 1.4 1.2 1.0 .8 .1 -.4 -.6 -2-2 Ni2

1-6 1.7 1.4 1.3 1.0 .3 -.3 -.6 -2-2 Ni3

9 1.8 1.3 1.3 .6 .0 -.4 -2.0 N:4

1.8 1.4 .8 .4 -.2 -1.7 NiS

1.9 1-8 1.0 .4 .3 -1.5 N:6

LINE : 1200 E


POLE-DIPOLE RRRRY

Dcrrx'VoiNT

N r 1. 2. 3. 4. ... •fi" SPRCING = 1 00.0 FEET


RED LflKE flREflOflTE i WINTER 1996 REF : 9602

SCflLE = l : 2400JVX LTD-

RESISTIVITY

12QQS (11DQS t l ODDS | 900S | BOOS | 7005 t 60QS t 5003 | 40DS , 30pS VHO") ~~""n-."i~ "M H fl)

Nil

N:2

N:3

N:4

43.7K

N:6

RESISTIVITY 4.2K Nil

N:2

N:3

Ni4

NiS

Ni6

MX CHG. MX CHG Nil

Ni2

NO

Ni4

Ni5

8.17*20

52N04SW0144 2 17420 DOME 240

Grid lPlate 3

LINE : O E

INDUCED POLflRIZfiTION SURVEY

POLE-DIPOLE RRRflY

N r 1. 2. 3. 4. ... "fl" SPHCING = 100.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND.GRID-1


SCRLE ^ 1: 2400

JVX LTD-

1600S 14(|OS , 130,05 , 120,05 100,05 , 90p5 , 80pS , 70ps , 60pS | 50pS i 40pS i 30pS , 20pS , lops , ON , IPpN | 20pN , 30pN , 40pN , 50pN , 60pN | 70pN , 80pN , 90pN lOqON , liqON , 12CJON , 13qON , 14qON 16(}ON , 17tjON 19qON , 20(}ON 2KJON

TflU THU

N:2

N:3

N:4

N:5

N:6

•3 -l -l .0 .0 .0 .0 .1 -O -l -O .0 v .2.0, -O -O N:l

•5 -l -l .1 .0 .0 .0 .5 .1 .0 -O .0 -5 .0 -O .0 Ns2

•3 -5 .3 .0 -O .0 1-0 .1 -l .0 .0 .5 .0 -O -O 1.0 N:3

• 5 -l -5 .0 .5 .3 1.0 -3 -l .1 .1 .5 -O .0 .0 .1 .0 N;4

•3 -3 .0 .1 .1 -O .3 .3 .3 .3 .5 .1 .0 .0 .3 .0 N:5

• 5 -3 -O .1 .3 /2tf^^tt^\ . 3 .3 .3 .5 .1 .1 .0 .1 .0 N:6

16QOS 13qOS , 120,05 , liqOS 90pS , 80pS | 70pS 40pS 20pS , IQpS , ON , 10pN , 20pN , 30pN , 40pN t 50pH , 60pN t 70pN 12qDN | 13qON , 14qON 17ON 19qON , 20qON , 2iqON

SPECTRflL MNil

N:2

N:3

N:4

N:5

N:6

221.8 336.8 /52.9

340.1 2X1-6 .827.6*,'

279.3

4.0, 200.9 171.0 183

168.1 183.7

5.6 165.4

.3 160.1 194.6^^^\\

'86.4 IB'7.6 159-3 188-5/^76.4 35).2 60.7

166^5 159.6 191.7/^1.2 5V^3/ 53.7/^34.1

.8 149.4 119.3. .44,8 . 62.4 48,1 .16.9 13.9

l 64.3 65.4

50.3 67.5 62.6 59

15

121.7 l

l 128.9 120

07.4 .85.7

''106.7 "

120.1 96/

.3 109.4

14.7 102.

2 115.3

,7*4 33.4

38.0

llSfl101?4 96.4

SPECTRflL M Nil

Ni2

N:3

N:4

N:5

N:6

LINE : 300 E

INDUCED POLflRIZfiTION SURVEY

POLE-DIPOLE RRRflY

DEPTH POINT

N ^ 1. 2. 3. 4. ..-

•fl" SPflCING - 1 00.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND-GRID-1


SCflLE - 1 : 2400

JVX LTD-

14(OS 90pS 70fS , 60pS 40pS , 30pS t 20pS 20pN , 30pN t 40pN , 50pN , 60pN 70pN 90pN , IQtjON 12()ON , 13qON , 14qON . 16(|ON , 17qON , ISqON , 19(jON , 20qON , 2iqON 230^ , 24CJON , 25qON . 26IJON 27qON

TflU8-0

N:2

N:3

N:4

N:5

N:6

O 8^ 4-0^ 2-0 4-0 i^^ 4.0 2-0 ^-OJS 1-0 .3 -O I-O .5

O .0 -O .1

-l .0 .0 .3

O .5 .0 .0 m.o .o .0

TflU -O N:l

N:2

N:3

N:4

N:5

N:6

ISQOS 13^03 | 12QOS t H OPS t 1 0QOS | 90pS i BOpS | 70pS , 60pS 40pS | 30pS i 20pS 20pN [ 30pN t 40pN | SOpN | 60pN | 70pN g B OpN , 90pN 120ON MÔN , IStjON 19qON | 200| OH i 2 10| ON | 220| ON | 23^ t 2 40| ON | 25(jON 2600N 27QON

SPECTRflL MNsl 230.8-1000.0 172,5, 234.1. 458.1__341.6 398.2 264.2 265.9

N:2 176.5 l

Ni3

N;4

N;5

N:6

189.

y 30.2 23.1

291

136^4 141.1 .277.1. 299.8 -633.1 137.7 124.4 8SPECTRflL M

N:l

N:2

N:3

N:4

N:5

N:6

LINE : 600 E


POLE-DIPOLE flRRflY

H = l . 2. 3. 4, ... *H" SPHCING = 1 00.0 FEET

FREEWEST RESOURCES

MCKENZIE ISLflND.GRID-1

RED LflKE flREflDflTE i WINTER 1996 REF : 9602

SCfiLE - l : 2400JVX LTD.

TflU

N:2

N:3

N:4

N:5

N:6

14QOS 13DOS | 12QOS HOPS l OOPS 9005 80QS 70pS | 600S t SOpS | 40pS | 30ps | 20pS t lOps [ Of) | IPpN [ 20pN | 30pN t 40pN | SOpN t 60pN 70pN g BOpN | 90QN | 10QON | UPON [ 12qON t 1 300N | 14qON | ISqON | ISqON | 17qON | IBqON 19qON | 20QON 2iqON | 22QON | 23QON 24QON

B O 16J) - 1. 2-0 Z.. - . ^

250[ ON | 260| ON | 27(|ON | 2BO| ON | 2900N

-O ^ 48-0 1&- 5 .0 .0 .1 .0 .0

.0 -O .0 .0 -O .0

O .0 -O .1 .1 -O -O -O

-O// .0 .0 .0 .0 l .0 -O .0 .0 -O .1 .0 -O -O -O

.0 .0 .0 .0 .0 .0 .0 .0 .0 .0 .1 .0 .0 .0

-o .o -o .o .o .o -o .o -o .o -i .o -o -o

TflU N:l

N:2

N:3

N:4

N:5

N:6

140,05 ,130,0s t 12qOS 90pS , 80pS , 70D5 , 60pS 40pS , 30pS , 20pSflu ''

ci OM

N , 20pN , 30pN , 40pN , 50pN , 60pN , 70pN , 80pN T 90pN , 10()ON , HCJON , IZCjONfl"

N , 17()ON 2i qON 23qON , 24(]ON , 25CJON . eeqON | 270| ON 2800N 2900N

SPECTRRL M225.4 273-3 262-9 233.3 279.6 240-6, .88^4^105.9

N:2

N:3

N:4

N:5

N:6

289.1 299-4 238-2 300

i.3 /266-325. .3 296-

271.8 yg&.Z 3 64.4

332-1 379.5

394.0

31^.8 406.1 257^^09.0 354.3 258.2 fl9

" 450.4 467.4 446.8 355.3 2^2.2 19J.8

6 465.0 463.1

408

3 428.5

481-9 460.7

.0 470-1 5 J(L^ 2 97

408-5 500.1 316-

2 ^18.0, 23.1 V8.32i).6 29.7

25.2 22.4 25.4

3 30-3 ^,28-Q 23.6

28.4 34-6

22

9.6

1.0 35-7 42.3

31-5 33-9

SPECTRflL M N:l

N:2

N:3

N:4

N:5

N:6

LINE : 1200 E


POLE-DIPOLE flRRflY

, NO . R ,

•-HD, ^

DCPTH'VaiNT

N r 1 . 2. 3. 4. ... "H" SPHCING = 1 00.0 FEET



SCflLE r 1 : 2400JVX LTD.

1200S HDDS lOqOS 90pS 80pS TODS 60pS 50pS 40pS 30ps

TflU TflU N:l 8.0 16.0 16.0 JÔ -1 4-0 ^2.0 1.0 2-0 1-0 N:l

N:2 16-0 ^̂ ^^-^^ 1 ' 0 ^— -^^y 4 " 0 \U 0 {ZÔ^/l- 0 N s2

N:3 . ^2' . 0 -0^^^ "^-O^Viis.^ . \ N :3

N:5 -0 ^^V^1^/^^^ ' 0 ' 0 N S5

N:6 .0 J^^^^^ff -0 -0 N:6

1200S 11QOS 1000S SODS 80PS 70Q5 60PS 50QS 40QS 300ST —— i —— 3 —— i —— ̂ —— i —— F —— i —— F —— i —— F —— i —— F —— i —— F —— i —— F —— ' —— T

SPECTRflL M SPECTRflL M N:l 266.3 421.7 y 58,7 43-3 37^ 306-9 265-1 234-3 213-7 199-9 N:l

N:2 395.2 lâ^Â^^^^5^^.Z\^2^. 1 32a*Tcg37.7 230-2 N:2

N:3 . Q-^^^.O .̂ VM^.4 /T^SÂz. 3 Sw7^2 — *33^8 N:3

Ni4 .0 .0 fflj^l T'^^^^^^^\ (ÔK N' 4

NiS .0 •0:^^v^^3.0^n) .O^Q\.6 Ni5

Ni6 .0 ^fl ^ — HJ ———— .0 ;^ Ni6

52N04SWD144 2 17420 DOME 250

Grid lPlate 3 a

LINE : -1500 W

INDUCED POLRRIZflTION SURVEY

POLE-DIPOLE flRRflY

Z?]___fl.

Dtrin'raiNTN r I. 2. 3. 4. ...

•H" SPHCING - 1 00.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND. GRID-1

RED LflKE flREflOflTE s WINTER 1996 REF : 9602

SCflLE - 1 : 2400

JVX LTD-

legos nqos isqos , isqos 14903 , isqos , i2qos ; iiqos , logos , aops , sops t vops , sops , jops 40ps , aops zîps tops i op i iopN t 20pN t aopN , 4opN t sopn sopN- — -~ -— — — — - — —-— — — - — ——

RESISTIVITY72.0 81.0 99.0 139.0 153-0 212-0 205.0 258-021,2- 3,OK 3-7K

N:2

N:3

N:4

N:S

N:6

123-0 148-0 178.0 172-0 2^.0 262

239-0 32190.0

272.0 223.0 230.0 239-0 299-

260-0 263.0 256.0 31^xtn 243

308.0 291.0 3*fTo 272.

297

I/^T)^

247

RESISTIVITY N:l

N:2

N:3

N:4

N:5

N:6

12qOS | li 90pS i 80pS t 70pS , SOpS

MX CHO.Nil

Ni2

Ni3

N:4

N:S

N:6

.1 .1 -.2 -.2 -1-2 -1.1 -1.9 -2.7

.2 .1 -.7 -2-1 -2-7 -3.7 -4-8

.0 -1.2 -3-0 -4.7 -6-3 -6.8 -7.7

-.8 -3.5 -6-2 -8-7 -8.8 -8-6

-3.6 -7.0 -10.0 -10-3 -9.2 -6-4

-7.6 -12-0 -11.8 -9.4 -5-9

-5.9

40s IPpS pN t 20pN , 30pN N t S OpN

-6 -9.0 -10

-8.2 -9.1 -

-8-1 -5-2 -28

J 1.6 -.3 -.7 -.5 -.5 -1.7 -1.5 -.3 -1.6,,,.10,2 11-1

3 -1.0 -7 -.8 --8 -.7 -2-1 -2-3 -1.8 -1.4/^TD^ 11-2

-.8 -2-8 -O -.8 -.9 -2-3 -2-5 -2.2 -1.6,^VO 11-1

O -4-6 -3-2 .0 -.8 -2.4 -2-6 -2-3

16-4 -4-9 -3-0 -.1 -2.3 -2-8 -2.5

4 -14.4 -3- T -2.0 -1-6 -2.7 -2-6 -.9

11.3

11.6

11.8

MX CHG. N:l

N:2

N:3

N:4

N:5

N:6

LINE : -1200 W


POLE-DIPOLE RRRflY

RESISTIVITY

legos | nqos i isqos i isqos nqos i isqos i i 2qos | iiqos t logos i gops t aops t 7ops r sops i sops t 4ops , 3ops 20ps i t opsJTs2. ''' .--.--. -j^

89-0

20pN , 30pN , 40pN 60pN

fl.

N : l . 2. 3. 4. ... fl" SPHCING = 100.0 FEET

N:2

N:3

N:4

N:5

N:6

RESISTIVITY N:l

N:2

N:3

N:4

N:6

MX CHG-

isqos t nqos i isqos j isqos f uqos , isqos t i 2qos ,iiqos ,logos t gops t aops , 7ops , sops i sops , 4pps . sops 20ps t tops*!"T- s

IQpN | 20pN , 30pN N , 60pN 70pN


RED LflKE flREflOflTE : WINTER 1996 REF : 9602

N:2

N:3

N:4

N:5

N:6

.2 -2-3 -.1

-1.6

.4 .3 -.1 -1.2 -1.3 .6 1.0 .1 1.4 -2

.9 .2 -1.0 -1.3 .7 1.4 .2 l

.8 -.7 -1.0 .9 1.7 .4 1.5

-.1 -.7 1.2 2.0 .4 1.7/^

-.1 1.6^/2.4/v .4 1.9 .1

2.l/ 2.8 f . 7 2.0 -.1 2

-2.8 -.6 5. 11.4 21^ 9.0

-.9

MX CHO. N:l

N:2

N:3

N:4

N:5

N:6

SCflLE r 1: 2400

JVX LTD.

LINE : -900 W


POLE-DIPOLE flRRflY

N r 1. 2. 3. 4. ... "R" SPflCING = 100.0 FEET



SCflLE r Is 2400

JVX LTD.

RESISTIVITY

legos t nqos , legos t i sqos i nqos , isqos , 12^05 , nqos , logos , gops aops , ?ops t eops t sops , 4ops ^sops ^P5 , 1 0PS , Of t 1 0PN , 20PN , 30pN i 40pn i sopN . eopN ?o

941.0 546*0 480-0^654.RESISTIVITY

N:l

N:2

N:3

N:4

N:5

N:6

MX CHG.

N:2

N:3

N:4

N:5

N:6

S t SOOS , 400S , 30QS , 20pS t 1 00S N | 30pN | 40pN11QOS 10QO1800S 17QOS

S.l. 1.4.9 . 28-5 .25.0 ,17 5.6 4-3. 2.7 1.3.3 -2.5 ...6v3 8.0 1.1-0 .19-2. 26-5 .15.3 14.0 l

5.3 4.5 4.2

10.S/ 6-

11-1 f 8 -1

LINE : -600 W


POLE-DIPOLE flRRflY

f^•*. e*vvrm mm

N r 1. l , 3 . 4."fi" SPflClNO s^lTJO.O FEET



SCflLE r 1: 2400

JVX LTD-

isqos i nqos , isqos T isqos^ nqos , isgos , i2qos i iiqos i logos , gops sops , 7ops i eopsRESISTIVITY

449-0 433,0 664*^X546.0 577-0 567.0 523.0 47S.o33-rfl

RESISTIVITYN: l

N:2

N:3

N:4

N:5

N:6

isqos nqos , legos , isqos , uqos i3j|os , izqos , n(|os , logos , sops , eops . ?ops , eops , sops . 4pps sops , 20p5 , tops ^ op , iopN , zppn ...30PN . 40PN . SOPN , SOPN , 70PN , 80PNMX CHG.

h-1 n-5

LINE : -300 W


POLE-DIPOLE flRRflY

SVDEPTH POIMT

N r 1. 2. 3. 4. ... -H" SPHCINO r 100.0 FEET



SCflLE r 1: 2400JVX LTD.

2011.4 13

4.8 23.8 16.9. 10-3^.10.5 14.1 13-1 10.1 14.8 14,8

MÎIT", T-1 M X CHG5 l.l 1.3 1-3 1.3 1.3 1.5 1.3 1.4 1.3 1.2 1-2 1-5 1.7_,2-Q 2-1 1.9 2-1 ^.2-9 3-3

3.17420

nqos legos isqos uqos isqos izqos nqos logos gops , sops , 70ps , eops sops . 40ps , sops 2ops tops , op iopN^ ̂ 20pN , sopN , 4opN , sopN , eopN , 7opN , 800J4 - ,J"P-N-L1 "(]0^ - | 1C1QN - 1 2tP 1 3(ION isqoN

RESISTIVITYn'5 n^6

N:2

N:3

N:4

N:5

N:6

19604^^95.0362^0 23^-0203RESISTIVITY

N:l

N:2

N:3

N:4

N:5

N:6

17QJ isqos 14905 ISQOS i2qos iitjos , logos , gops

j-p-3*

S 70pS i 60pS , SOpS | 40pS t 30pS , 20pS op . iopN . 20pN , sopN , 40pN . sopN i sopN . 7opN . 8opN gopN i2oN uqoN , isqoN . leqoN , nqoN , leqoN

MX CHG.N: l

N:2

N:3

N:4

N:5

N:6

4-5 4.8 4-Q ^2-4 2-4 2-5 2.4 2-0.^1.6

2.6

n-'S S Û- (62, T- 2(3) ^-2-0 2.92-2 2.1 2-3 2.1 2-0 ^1.9 1.4 LO8 . 4.1 . 7.0 6.8 7.4 6-2^ 4.4

3-9 5.8 5.1

13.2 14.4 11.1 11.2 10.6

9.1 8-1 7.7 6.7 7-0 7.8

9.3 8-9 8.4 7-7 8-7

8.8 6-4

8.2 6-6 9.5 7.Q

MX CHG. N-.l

N:2

N:3

N:4

N:5

N:6

O (D CM

Grid lPlate 4

LINE : -1500 W


POLE-DIPOLE RRRRY

\ VoertH POINT

N - l . 2. 3. 4. ... •fl" SPflCING ^ 1 00.0 FEET



SCflLE - 1 : 2400JVX LTD-

TflU

N:2

N:3

N:4

N:5

N:6

SPECTRflL M

N:2

N:3

N:4

N:5

N:6

ISQOS , i7([os legos isqos , uqos 1 1 3^05 1 12^03 , iiqos , logos . gops | aop5 | 70ps .eops , sops , 40ps i sops i zops , tops iopN , 20pN i sopN i 40pN , sopN i eopN

TflU 2.0 Nil

legos , nqos , isqos i isqos , uqos , isqos t i 2qos | nqos t logos , gpps , sops , 7ops , eops , sops t 4pps sops t 20ps , iops , ON 20N 40pN

.0 .0 ^g.8 4.4 -19.7 -15.6 24-1 -35-1

.0 -10.2 'flFa.. -34.3 -47-8 -62.6 -75W ^ *~^JSf . 0 -38.9 l^p .1) -78.8 -85-2 -95-8

.0 -46.2 -78.4 -107.9 -108-8 -106-6 -86

-48.1 -88.3 -127.7 -127.0 -115-2 -82-9

-94.8 14AS3V-148.4 -116-3 -79-7 6,

•3 4J)K,y2.4 -23-3 -21-5 4.9 -41.

VoTffr^qPKl -27.2 -30-6 -23-4 Ms&Z

.4 144.6

SPECTRflL M N:l

Nt2

N:3

N:4

N:5

N:6

LINE : -1200 W


POLE-DIPOLE RRRRY

DEPTH "

N - 1. 2. 3. 4. .-.

H" SPRCING s 100-0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND,GRID-l

RED LflKE flREflDflTE : WINTER 1996

SCflLE - 1 : 2400JVX LTD-

TRU

N:2

N:3

N:4

N:5

N:6

SPECTRflL M

legos i nqos t teqos | isqos i uqos , isqos t i zqos iiiqos , logos i sops i apps , 70ps t sops , sops t 4cps , sops i 20ps i lops , ON , iopN | 2opN i sopN i 40pN t sopN i eopN i 7ppNTRU

.o .o .o...ia.o. ..4 •o .1 .o .o

.1 .0—— .3 .0.0 .3 -O -O

.0 .0 .0 -O .0 .0

.0 .0 .0 .0

.0 .0 .0 .0

1800S | 1700S | 16QOS t 1SOOS ( 14QOS 13QOS , 1200S i H OPS | 10QOS , 90DS | 800S 7QOS | 60pS . 50pS t 40pS [ 30pS | 20pS | IQpS | ON | IPpN t 20pN | 30pN t 40pN t 50pN | 60pN t 70pN

SPECTRflL M ,253.0 136.6 N:l

LINE : -900 W


POLE-DIPOLE RRRRY

N - 1 . 2. 3. 4. ... fl" SPflCING - 100.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND,GRID-1

RED LflKE flREflDRTE : WINTER 1996 REF : 9602

SCflLE r 1: 2400

JVX LTD-

TflU

N:2

N:3

N:4

N:5

N:6

isqos i nqos , legos t isqos , uqos , isqos i i 2qos , iiqos t logos t gops , aops , 7ops , 60ps i sops , 4pps i sops i 20ps , tops | ON t iopN t 20pN , sopN , 4QpN , sopN t eopN t 70pNTflU

48-0 N:l

N:2

N:3

N:4

N:5

N:6

-l 1.0 .1 l

nqos t legos t i sqos 114(^05 , isqos 112^03 i nqos tioqos i gops , sops , 70ps sops , sops , 40ps , sops t 20ps t l ops t op t i opN i 2ppN i sopN t 4ppN , sopN t sopN t 7gpN

SPECTRflL M

N:2

N:3

N:4

N:5

N:6

99.9 137.4| 221.7 294.4 189^4 170-1 195SPECTRflL M

N:l

N:2

N:3

N:4

N:5

N:6

LINE : -600 W


POLE-DIPOLE RRRflY

N s 1. 2. 3. 4. ..."fl" SPflCING = 1 00.0 FEET



SCflLE = 1: 2400

JVX LTD.

TflU

leqos i nqos , legos i isqos i uqos i isqos 112^03 t t iqos t I OCJQS i sops i aops i 7ops t eops i sops , 40ps t sops i aops i lops

4.0 . .0 -O .0 -O -O ... 4-0. ... -5 . .2.0 2-0 . 2-0 . 4-0 . 2-Q 20. 4-0

3N t IQpIQN 30pN | 40pN t 50pN , SOpN | 70pN | 80pN t 90pN nqoN i isqoN

N:3

N:4

N:5

TflU .1 -5 -l -l -O .5 -O .3 -O N:l

.1 .1 .1 .1 -l -l .3 .0 N:2

•S .0 -l -l .1 .1 -l .1 N:3

.3 -O -l .1 .3 -l .0 N:4

•3 -l .0 .1 .1 .t .0 N:5

.1 l .1 .0 N:6

isqos i nqos , legos i isqos i nqos t isqos 1 120^5 i iiqos , logos i gops , sops t 7ops i sops . sops , 4ops . sops i zops L lops t ON i iopN i 20pN t sopN t 4opN [ sopN i eopN i 70pN t sopN ( gopN N T 12^ t isqoN UPON ISOON , IBQON nooN i ISQONSPECTRflL M

45.1

N:2

N:3

N:4

N:5

N:6

126.6 129-0 . 170-3 157.3. 124.4 176.1 178-2 15.0 17.7 17-9 17.5 17.4^.20.1 16.8 17.9 16.8 15-7 17.2^^19.7 26.9, 30-6 36-1 S ———————————————-———————— ————————————^^————————-^^- ^-0^

4 24.4 26.0 28-4 29.0 25.9 26.5 25-4 24.7

142

-2 35.5 38.6 33.7 32-9 TTT*

2 48.8 43-7 43-9 41-0 38-3 37-5 36-3

45.3 44.7 42-1 42.4 42.

61-7 S3.r\49.2 48-0 46.4 47.3

81

84.8 93-6

80-2 81.3 lltf.8 159.3

-6 92.1 ^rfS.2 16CX6

99-4/124.7 106^8

SPECTRRL M N:l

N:2

N:3

N:4

N:5

N:6

LINE : -300 W


POLE-DIPOLE RRRRY

- l

N = 1. 2. 3. 4. ... "fl" SPflCING - 1 00.0 FEET


RED LflKE flREflDflTE s WINTER 1996 REF : 9602


2.1742015CJOS 90pS 70S SOpS t 40pS ( 30pS t 20pS ON | 10pN 30pN | 40pN 90pN t 1C(|ON 12(]ON 17QQN | I800N 19QON

TflU TflU

N:2

N:3

N:4

N:5

N:6

2-0 . 1.0 . 2.0 . . .5 l .0 ^ l .0 . 2-0 . . .5.5 .3 .1 -l 2-0 . 1.0 , 2.0 2.0 2-0, , .3 .3 -l .3 -O .0 .0 -O .3 .Q .Q .o

1-0 .5 .3 -3 2.0^ 2.0 2.0 2-0 / ^ .3 .5 .0 -l .0 -l -O

ri-o__i.o i.5 .5 .3 .3

.5 .5 .5 .3

1.0 -5 .5 .5 -5 .s i.\o r.q f re1-0 .5 1-0 • O /I.O 1-0

2.0

1-0

1.0 1.0 -5 .5 .5 l

.1 .0 .0 -l -l .1 .0

.1 .1 .0 -l -l .1 .0

.1 .0 .1 .1 .1 .3

l .0 .3 .0 -l -l

N:2

N:3

N:4

N:5

N:6

90pS t 80pS | 70pS | 60pS 40pS t 30ps t 20pS N i IQpIQN 30pN | 40pN 60pN | 70pN 80pN | 90pN | 10C|ON 15C|ON | 1600N i 1 7QON | 18QON i 19Q ON

SPECTRflL M

N:2

N:3

N:4

N:5

N:6

58-9 60.3 51-4 31.2 31.3 36.9 32-3

51.3 73.S 64.8

50.2 ?'l.l^^7^ri^^64.2 67.5 67

80.9 94.7 88.0

'O/ 117.0 110.7 108-1 -"-89.8

78.9 51.2

122-1

31.9 128-6 120.3

138.0 130.5 116

141.0 137.2 125.6

139.8 130.1 100

4.6 28.1^28^7 30.2 .2JL-0 26.2 24-2

38.4 40.7 38.5 35-8 34.

47.1 45-4 42.5 39.7 35-1

53.1 SIT*-^ 48.1 45.8 42-5 38.0 35-3

64-8 57.1 53.7 SIS^ 46.7 42.7 41.1 37-1

68.4 59.0 56.1 53-5N47.8 45.4 42-2 43.0 8 118.6 133.9 100-2

SPECTRflL *

Ns2

N:3

N:4

N:5

N:6

O N. CM

Grid lPlate 4a

o oCO

O O

O O (M

O O O

o oOD

O O CO

O O

O O CM

UJ CO CC CD

O O (M

O O

O O CO

LU

O O CO

UJ

O Oo

UJ

o oCM

UJ

o o o

oCD

2400 N 2400 N

1200 N

O

300 S

600 S 600 S

900 S 900 S

52N04SWD144 2.17420 DOME 280

1800 S 1800 S

o oCO

o o

o oCM

o o o

o o00

o oCO

o o

o o(NJ

UJ

LU COcr03

UJ

ooCM

UJ

o o

o oCO

UJ

o oCO

o o o

UJ

o oCM

FREEWEST RESOURCES CANADA INC.

MCKENZIE ISLAND PROPERTY - GRID zRED LAKE MINES and MINERALS DIVISION

______________N.T.S. 52 N/4 ___________-

CHARGEABILITY CONTOURS (11=2)CONTOUR INTERVALS : 2 it 1 0 mV/V

TIME WINDOW 310-1050 ms


WINTER 1996

200 400 600

PLOTTED BYA.S.

FEB. 1 996SCALE 1 :2400 PLATE l

JVX ref. no. 9602

LINE : -1200 S


POLE-DIPOLE RRRflY

ffl.

acrm'nunN : 1. 2. 3. 4. ...

•R" SPflCINO = 1 00.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND,GRID-2


SCflLE = 1: 2400JVX LTD-

RESISTIVITY

MX CHO.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

1300N 12QOH , IIQON , 1000H , 900H , 80QH1 * * 60QH 40 VofP"d(A 0p"dl\ 10pH—"E-'-'.gPJ-'JiT 30 P E - 40 P E 50P E

6K

RESISTIVITY O N:l

N:2

N:3

N:4

N:5

N:6

OE , IPpE , 20pE , 30pE , 40pE , 50pE

MX CHG. 5.,l 8.2 N:l

N:2

N:3

N:4

N:5

N:6

LINE : -1500 S


POLE-DIPOLE flRRRY

DEfTM'VoillT

N r 1. 2. 3. 4, ...

'IT 8PHCING ^TTJOTQ -Hit T



SCflLE r 1: 2400JVX LTD-

90HpH | 80pH | 70pN | 60J3H 2DpE . 30pE 40pE | 50pE

RESISTIVITY

N:2

N:3

N:4

N:5

N:6

7K

9K

RESISTIVITY N:l

N:2

N:3

N:4

N:5

N:6

MX CHG.

90H 80H

-3.5

20pE . 30pE , 40pE , 50pE

MX CHG. N:l

N:2

N:3

N:4

N:5

N:6

LINE : -1800 S


POLE-DIPOLE flRRflY

V'DEPTH POINT

N = l, 2, 3, 4 . ...

"fl" SPflCINO - 1 00.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND-GRID-2



20pE . 30pE 40pE { 50pE

RESISTIVITY

N:2

N:3

N:4

N:5

N:6

RESISTIVIT N:l

N:2

N:3

N:4

N:5

N:6

20pE : 30pE : 40pE | 50pE

MX CHG.

N:2

N:3

N:4

N:5

N:6

X CHG. N:l

N:2

N:3

N:4

N:5

N:6

O O) CM

Grid 2Plate 7

LINE : -1200 S

INDUCED POLflRIZRTIQN SURVEY

POLE-DIPOLE flRRRY

ffl.

N s 1. 2. 3. 4. ... •fl" SPHCINB s 100.0 FEET

FREEWEST RESOURCESMCKENZIEISLflND, GRID-2



13(OH13(] 80pH SOpH H | 20pH IQDE | 20pE , 30pE , 400E , 50PE

THU TflUNil

N:2

N:3

N:4

N:5

N:6

13(OH 12(DH 90H SOpH 20pE ; 3QpE | 40pE

SPECTRflL M

N:2

N:3

N:4

N:5

N:6

SPECTRflL M 6 N:l

N:2

N:3

N:4

N:5

N:6

LINE : -1500 S


POLE-DIPOLE flRRRY

DEPTH'ValMT

N r 1. 2. 3. 4. ... •H" SPHCING = 1 00.0 FEET

FREEWEST RESOURCESMCKENZIEISLflND,GRID-2



H i 70pH u | 40pH | 30pH , 20pH IQpE | 20pE . 30pE , 40pE

TflU TflU.1 LO

N:2

N:3

N:4

N:5

N:6

l .3 1.0 .3

N:2

N:3

N:4

N:5

N:6

80pH t 70pH | 60pH 40pU | 30pH 20pE . 30pE , 4ppE [ 50pE

SPECTRflL (1

N:2

N:3

N:4

N:S

N:6

SPECTRflL M 51.2 N:l

N:2

N:3

N:4

N:5

N:6

LINE : -1800 S


POLE-DIPOLE flRRflY

N s 1. 2. 3. 4. ... •fl" SPRCING :; 100.0 FEET



SCflLE - 1 : 2400

JVX LTD-

20pE , 30pE , 40pE , 50pE

TflU

N:2

N:3

N:4

N:5

N:6

90pH , 80pH | 70pH , 60pH 0pH 10pV4 , 20pE | 30pE , 40pE { 50pE

SPECTRflL M

N:2

N:3

N:4

N:5

N:6

51

60

SPECTRflL M N:l

N:2

N:3

N:4

N:5

N:6

O O CO

Grid 2Plate 7a

LINE : O N


POLE-DIPOLE RRRflY

-0,

OtPTH POINT

N r 1. 2. 3. 4. ... •R- SPflCIMO - 1 00.0 FEET

FREEWEST RESOURCES



SCflLE r 1: 2400

JVX LTD-

TRU

Nt2

Nt3

N:4

N:5

N:6

SPECTRflL MNil

N:2

Ni3

N:4

N:5

N:6

80pH 60pH 50pH , 40pH —— 30pH i 2DpM IQpH OE 20pE 30pE , 40pE , SOpE 60pE 70pE 80pE i 90pE , IQtjOE 12()OE , 13qOE | 14()OE

4-0 . 2,0 2-0 N:I

48.0 \\ V O .0 .3

.0 -O .3 .5 -3 -O

80pH , 70pH M 30pH 20pH OE , IQpE 20pE 30pE 40pE , 50pE 60pE , 70pE , 80pE | 90pE 12QOE , 1300E L 1400E

24-1 25.5 27.8 27.4 l 122. .9 142.4 170.5

-40.3

292.1^78.5.9, 1 39 - 7

279.3 27L8MOOO.O

'/m 249.7 23Ts2

281.^447.0

l

C^B^rHlS -4

SPECTRRL M N:1

N:2

N:3

N:4

N:5

N:6


POLE-DIPOLE RRRflY

fi.\ .' V

DEPTH POINT

N - L 2. 3. 4. ...

•fl" SPflCING r 100.0 FEET

FREEWEST RESOURCES




H , 121JOH H , 7DpH | 60pH , SOpH , 40pH [ 30pH OE , IQpE | 20pE t 30pE , 40pg , 50pE , 60pE , 70pE | 80pE | 90pE 12(}OE 1400E 16qOE 17qOE

TflU4-0 . 2..0 v LO LO

N:2

N:3

N:4

N:5

N:6

8.0 .1 .5 .5 LO ,1,.0

.1 .5 LO J l .t^T~

O -3 -S LO LO

.5 .5 .5 LO .5 LO .5 LO l -0,^, LO

.5 -5 .5 .5 .5 LO .5 .5 MJ ,-

.5 li

.4-0

.5 .5 .5 .3 .5 LO .5

TflU O, 16.0 N:l

N:2

N:3

N:4

N:5

N:6

SPECTRRL M

| 13qOH t 12Q.OH { HOOK IpqOH | 90pH , 80pH | 70pH t 60pH t 50pH , 40pH | 3DpU i 20pH , 10pH , OE | IPpE i 20pE 30pE , 40pE , 50pE | 60pE | 70pE t 80pE t 90pE , IQCJOE , HOPE , IZÔE t 13(]OE | 14C|OE | ISqOE t IStjOE | 17CJOE

N:5

N:6

o ^—— -^ 74.6 95.2 /i(5feQ3 78-5 d23-6 130-7 116.3 102.2 122.7 136.3 112.0 124.1 119.0

72.0 1021.4/84.4 85.3\ 141.-.3 145.1 127.8 110.1 141.0 152-1 125.5 121.5 115.3 125-6 114.5 138

61.7, 103..5 123.5

106.4 127-0

.1 5L5 56.7 59-7 73.4 299-6

1.3 W.B-224.

119.3

94-8 l-WL-6 125-8 10

3 87.5 9TV7 129.8 133.9 125.

84.1 84.6

77.8 80-• 2 llO.O 18L6 172.3

SPECTRflL M N:l

N:2

N:3

N:4

M:5

N:6

LINE : -600 S


POLE-DIPOLE RRRflY

fl.

OEPTH^POINT

N - L 2. 3. 4. .-. •fl* SPflCING - 1 00.0 FEET

FREEWEST RESOURCES

MCKENZIE ISLflNDpGRID-2


SCflLE = 1: 2400

JVX LTD-

1700H 12QOH 40H | 30U | 20H . OE | 10pE \ 20pE t 30pE , 40pE 70pE i 80pE t 90pE

TflU

N:2

N:3

N:4

N:5

.0 .0 .0 .1 .0 .3 -5 -O LO .3 ^.0 -3 .0 .5 LO 1^0 v 2-^—— L

'• 0 ^v^y/ft v 4 ' 0 \VyLO LO rs-fl— \ LO l V-ffj 4.0 ^^D-~^

8.0 8.0 ^ 4.0

.0 .0 .1 .3 -l .5 .5 LO 1.0 —— 1-0 .1 -S

.1 .0 .3 .5 .3 -l 1.0 1.0 1.0 .5 .3 1.0 .5 LO .5 .5

.0 .0 .5 .5 .3 LO .5 .5 .5 .3 LO .5 .5 -3 .5 LO LO

.3 .0 .5 .1 .5 .5 .5 -5 -l LO -5 -5 -l .3 LO .5

.1 .1 .3 1.0 .5 .5 -5 .1 .5 —rS— —^J -l———-rt .S .0

-' -L'j ^Jo^ - ~~~

8.0

LO

TflU 2-0 N:l

N:2

N:3

N:4

N:5

Ni6

90pH 60H 40H 30U 20H IPU OE 10E 2QE 30E 4QE 60E 80pE | 90pE t I QCJOE 14(OE

SPECTRflL M33-9 33.3 43.9 44.8

N:2

N:3

N:4

N:5

N:6

20

20-5 23.1

25.5

44^8 59.,8 106.1 113.2 H8

T80 oM2.4 123.0 132

.9 125.7 130.6

128.1 129.3 128

•7 130.1 128.7

255 7 300.5 306^6,^15.3

284^0 367. 5o 206.7^0346 — o o

202-4 288.6 219.5 O35L5 32i\B 247.1

611

371

.9 417

SPECTRflL M -3 .264.0 , 153.6. 283.9 153-8 N:l

N:2

N:3

N:4

N:5

N:6

LINE : -900 S


POLE-DIPOLE flRRflY

DEPTH'*'rOIMT

N r 1. 2. 3. 4. ... •H" SPRCING = 1 00.0 FEET

FREEWEST RESOURCES




TflU

N:2

N:3

N:4

N:5

N:6

SPECTRflL M

N:2

N:3

N:4

N:5

N:6

H , 14qON 200H 30H OE , 10pE t 20pE , 30pE , 40pE 60pE t 7 0pE [ 80pE 9QpE t 10(}OE 12t|O

TflU.0 .0 .0 -O -O .0 .3 .0

.0 .0 -O -O -O .5 .0

.0 .0 .0 .0 -5 .0 LO

.0 .0 -O -l

.0 .0 .0 .3

LO -O -3 .0 8-0. 2.0 2-0 4.0 4.0 N:l

• O -5 -O .0

.0 .0 .0 .0

.5 .0 .0 -O

-O -O -O .0.0 .0 .0 -O -3 ^ ).

.0 .0 .0 .0 .0 .0 .0 .0 .1 .3 -O .0 -O -O -O -O

1700H 70H OE , IQpE t 20pE | 30pE t 4 0pE 60pE t 70pE t 80pE 90pE , IQCJOE , li

LOK,, -O,,. 15 13B..7 208.-6 426-8

j:s~-*e6.

SPECTRflL M N:l

N:2

N:3

N:4

N:5

N:6

7420

oCO

Grid 2Plate 6 a

LINE : O N


POLE-DIPOLE flRRflY

fl.N - 1 . 2. 3. 4. -..

•fl" SPRCING - 1 00.0 FEET




RESISTIVITY

Ni6

U 2DpH —— LOpH , OEH i 70pM , 60pH | 50pH 20pE , 30pE r 40pE , SOpE , 60pE 70pE , 80pE , 90QE 1000E , 1100E 1200E' ---61.3K 72.6K 28..0K

^TTR^,

N:l 133.0 85.0 62.0 56-0 65.0 86.0 170.p,,862.0 795.0 563.0, ,2

N:2 203-0

Ns3 154.0 328xKf^22l2lZ3?*^Lll?TrO—2*2TU285.0^^375.0X377.0| 863.0\ ]f.6K——l

N:4 210.0\ f ^"^-^ "———"^ i

Ni5 295.0\ 734.0 934.0 72?7TJ*--*62i0548.063*reN 549.0 704.0 \L1K\ 2\ x-——-—^ ———— V—**S

832395

RESISTIVITY 950.0 N:l

N:2

M:3

N:4

N:5

N:6

^M ~

IH 70pH , 60pt4 , SOpH 40pH 30pn 20pH IPpH OE , IQpE , 20pE , 30pE , 40pE SOpE 60pE , 70pE 80pE , 90pE , IPqOE , HOPE , 1200E ISqOE MODE

MX CHG. MX CHO-

N:2

N:3

N:4

N:5

N:6

2.1 2-3 2.6X ,4.5 B.7. ..31.5 23-5 29.6 16.3

L. l INC.


POLE-DIPOLE flRRflY

Z?]V'

DEPTH raiHT

N r 1. 2. 3. 4. ... 'H" SPHCING - 1 00.0 FEET



SCflLE r 1: 2400

JVX LTD-

1300H 70pH 20pt4 IQE 30pE , 40pE 60pE | 70pE , 80pE 12QDE 14 (|OE 16QOE , 1700E

RESISTIVITY453.0

N:2

N:3

N:4

N:5

N:6

09713

l.OK

l 697.0 864.0 882-0 455.0^58^0 191-0.^136

.0 615-(L 705-0 894-0 59g/S ""^-S.

572/0 494.0 ^B-0 941.

.0 \539-0 5 11.0 Sg2.0

756.0 666TD** COU8^ 857.

.0 971.0 848.0 754.0

11.8K

SK

4K

RESISTIVITY N:l

N:2

N:3

N:4

N:5

N:6

r P-

14QOH p 1300H | 12QOH 10QOH | 900H | 80pH 40pH 20pU | IQpH OE 70pE t 80pE , 90pE , IQCJOE | liqOE | 12QOE , 13QOE

MX CHG.

N:2

N:3

N:4

N:5

N:6

14-9

8.6 . 3,8, 1.9 2.3 , 3.4 3.2. 6-1 .2*6 2.4 1.7 2-7 2

10-2 ^6-3 6.0 5.2 S-SX' 6.8"S^ 5-1 5 -7^" 7 .2 8-5 \5-2 ^xC.7 7.8 10

7.0 6-7 7.3 ^6^3 7.6 8.4 7.1 7.0 8.9 9.4 7.4 8.3 9

5."S\ 7.6 8.0 6-2 9.7 ^---te-^L^ 9-1 8-0 9.6/îi'^J^s^ 8.8 9-8 9-5

5-^\ 8-2 6-5 6.7 li.l 11.5 ^Q.O 8.4 li.l 12-5 ^9-8 9.5 9

* o.

15QOE 17QO

7.7 9.9 4.9 4.0 4.4

6-7 6-3 7.5 \12-1 12-0 11.3

.5 5/8* ^r\.l 9-ft 13-1 13.3

MX CHG. N:l

N:2

N:3

Ni4

N:5

N:6

LINE : -600 S


POLE-DIPOLE flRRflY

Z?]____fl

N - l . 2. 3. 4. ... fl" SPRCING : 100-0 FEET



SCflLE - 1 : 2400JVX LTD.

1700U II OOH 30n OE 10E 30E 40E 70p 90pE 12CIOE

RESISTIVITY

N:2

N:3

N:4

N:5

N:6

^876-0 920.0 9j

896 O 1.3JS-——UgK 1.2K 1-2K l .3K

l.OK/ 1-7K -2.1K "M-SM——^ .SK 1 .3K

RESISTIVITY 24.IK N:l

N:2

N:3

N:4

N:5

N:6

1700H ISOOU 12QOH 90pH OE 20pE . 30pE

MX CHG.8.5 9.,l

N:2

N:3

N:4

N:5

N:6

10.6

.4 .2 .6 .5 -7 1.4, 2

.7 .4 .9 1.0 1-51-

1.0 .7 1.2 1.5/ 2.

1.2 1-0 1-7 y 2 -2

1.5 1.4 7 2-3 2-

1.7 119 2-7

4 13.0

11.3 12.5 12.9 14.2 12

9.8—-^.

.9 10-2 10.5 10.4 li.'

10.8 10.6 10.2 11.1 13'

.8 11.2 10.3 10-8 12-S"

21,5

10.8 f 1 9.5 16..^

18vl 25.

0 - X17\6 28.6

19.7 j)9.4 30.6(———121.7 22.3 27.6

MX CHG. N:l

N:2

N:3

N:4

N:5

N:6

LINE : -900 S


POLE-DIPOLE flRRRY

Ifl___fl.\ s

OErTH m l NT

N - 1 . 2. 3. 4, ... •R" SPRCING = 1 00.0 FEET

FREEWEST RESOURCESMCKENZIEISLflND, GRID-2

RED LflKE flREflORTE : WINTER 1996 REF : 9602

SCflLE - 1 : 2400

JVX LTD.

H 90pH SOpH , 70pH | eopu , SOPH , 40pU t 30pu 20pH

RESISTIVITY

10pE , 20pE , 30pE , 40pE , SOpE | 60pE t 70pE , 80pE , 90pE ~~ ~ 12qOE

N:2

N:3

N:4

N:5

N:6

109.0 126.0 147.0 95.0 93.0 118.0 J/76.Q 414,0

194 .fl^^52ôl^369^^?30ja—22^ ^?75jj)^-^58xO

308^\A3ô |2aIq^jHra^n 39a-a--^72TQ 501462.0^/692.0 986-0

674-0 98^0

902

4K

0 754 IK 2-7K

RESISTIVITY N:l

N:2

N:3

N:4

N:5

N:6

rp- 1TP-12QOE

MX CHG.

N:2

N:3

N:4

N:5

N:6

pE t 70pE ; 80pE . 90pE1400M 1300M 12QOU lf\-ivia,r-M-306, T

26.9 25 10.2 12-1 .4.a 7.6 5.85 .1 .2 .2

8.7 8VVH-1.6.0 .3 .4

-.1 .4 .7

MX CHG.14.9

28-8 26.0\19M 28-0

31-53TT5--^29.6 23-8

-4 34.9 33.9 34.5

37.8 37.0 34.8

N:2

N:3

N:4

N:5

N:6

742

Grid 2Plate 6

oCM CO

LINE : 900 N


POLE-DIPOLE flRRflY

ffl.

DEPTH'VaiMT

N - 1. 2. 3. 4. ... •fl" SPHCING = 1 00.0 FEET

FREENEST RESOURCES

MCKENZIE ISLflND.GRID-2 RED LflKE flREfl

DflTE : WINTER 1996 REF : 9602


15(jOH 4 14(|OH t 1 3(}OH , 12(]OH | 1KJOH | 10(|OH , 90pn 70pH 50pH 30pH OE , IQpE ( 20pE , 30pE t 40pE ( 50pE | 60pE , 70pE

TflUNil

N:2

N:3

Ni4

NsS

N:6

SPECTRflL hNil

Ni2

Ni3

Ni4

Ni5

Ni6

.5 .1 .0 .1 .0 .0 .0 .0 .1 .3 -3 .5 .3

.5 .1 -l -l .1 -l -l .1 -3 .3 .3 -S .5

.3 .1 .1 .1 .1 .1 .1 .1 .3 -3 .5 1.0 .5

.3 .1 .1 -l -l .3 .3 -3 -3 .5 .5 1.0 LxD 7 2 .0 2-0 2.0 2-0

2.0 2.0 2.0 2.0 2.0 2.0. .1-0

2-0 2.0 2.0 2-0 2.0

2-0 2-0 2.0 2 .1

.3 .1 .1 .1 .1 .3 .3 .3 .5 .5 1^0 C 2 .0 2.0 2.0 2.0^ ^0 1.0 '

.3 .1 .1 .1 .3 .3 .3 .3 .5 1.0 N.(K 2.0 2.0 2-0 2^0 A 1.0 l

——'J \1-r* * 1.0 N1.0

TflU 512.0 Nil

Ni2

Ni3

Ni4

NiS

N:6

13(|OH , 12CJOH IQCjOH | 90pH 70H 50pH 20pH , IQpH , OE t IQpE , 2QpE t 30pE 60pE | 70pE

2 40.

49.7 37.7 40.8 33.2 35.4 22.2 20.8 21.2 25.8,^28

4-0 41.4

.6 41.8 47-6^-6*

A9-J}——52.8 56.9

.6 61.7 61-3 66

75.0 69-3 72-4

.8 29.5 32.4 42

40.4 41

245.6 251.4 254.1 285.4 292.8

SPECTRflL M Nil

Ni2

Ni3

Ni4

Ni5

Ni6

LINE : 600 N


POLE-DIPOLE flRRflY

fl.\ *

OEPTH'VoiNT

N —— It t* di 4* BBI

•H" SPHCINB - 1 00.0 FEET

FREEWEST RESOURCES



SCflLE = li 2400JVX LTD.

90pH | 60pH , SOpH | 40pH | 30pM t 2 0pH 10pH t OE pE , 70pE , BOpE i 90p

TflUNil

Ni2

Ni3

Ni4

NiS

Ni6

2.0 - 5 - 1 - 0 ' 0 - 1 - 0 - 1 - 0

.5 .0 .1 .1 .0 .1 .0

.5 .0 .5 .5 .0 .0 .0 .1

.0 .5 1.0 .0 .1 .0 -3 .0

~"~~ -3 1.0 .0 -O -O .0 .0 .0

1.0 .0 .0 .0 .0 .0 .0 .0

.0 -O .0 Nil

Ni6

IQCDH BOpH , 70pH t 60pH 30pH , 20pN , IQpH , OE 20pE , 30pE , 40pE , SOpE , SOpE | 70pE , BOpE | 90pE

SPECTRflL MNil

Ni2

Ni3

NU

Nt5

Ni6

18.7 229.3 263,1 427.4.1,39.3 176.77 229.3 263.1 42

353^T*-304o-* 340.7 P.3' 81.8 106.4k o

43

353

•8 339.9 366.4 340-0 428.'

325.9 326.0 360.4 353.3 410-tb \M4^8 150-9

-O 323-3 320-8 409-4 392.2 401^^45.6

18-1 321.0 321.5 443.4 397.6 399.7

82.1 79.9SPECTRflL h

Nil

Ni2

Ni3

Ni4

NiS

Ni6

O CO CO

LINE : 300 N


POLE-DIPOLE flRRflY

^ f'

OEPtHHrolMT

N ^ 1. 2. 3. 4. ... •H" SPHCINO = 100.0 FEET

FREENEST RESOURCESMCKENZIE ISLflND.GRID-2


SCflLE = l: 2400

JVX LTD.

BOpH , 70pH , 60pH 40pH [ 30pH , 20pH OE ^ IQpE t 20pE , 30pE , 40pE | SOpE , 60pE , 70pE 90pE , IQIJDE

TflU

N:2

N:3

N:4

N:5

N:6

1KJOH t l OQOM t 90pH , 80pH , 70pH , 60pN , SOpH , 40pN | 30pH , 20pH ZOpE , 30pE | 40pE 60pE , 70pE t BOpE , 90pE , 10(|OE 12 CJOE

SPECTRflL MNil

Ni2

Ni3

N:4

Ni5

Ni6

10.9 19.2 18.6 18.7__17SPECTRflL M

109.0 Nil

Ni2

N:3

Ni4

NiS

Ni6Grid 2

Plate 5 a

LINE : 1800 N

INDUCED POLARIZATION SURVEY

POLE-DIPOLE flRRRY

N = 1. 2 , 3 . 4. .-. "R" SPPCINO r 100.0 FEET

FREENEST RESOURCES

MCKENZIEISLAND.GRID-2

RED LAKE AREADflTE i WINTER 1996 REF i 9602

SCALE r l s 2400

JVX LTD-

70pH , 60pH t 50pH , 40pH , 30pH , H | OE

TflU

N:2

Ni3

Ni4

N:5

N:6 .0 ^ .0

TflU N:l

N:2

N:3

N:4

N:5

N:6

60pM t 50pH | 30pH OE

SPECTRflL M62.4

N:2

N:3

N:4

N:5

N:6

SPECTRflL M 187.3 Nsl

Ns2

N:3

N:4

Ns5

N:6

LINE : 1500 N


POLE-DIPOLE flRRRY

DEPTH'VolNT

N r i. 2. 3. 4. ...

"H" SPRCINO r 100.0 FEET

FREENEST RESOURCES

MCKENZIE ISLAND,GRID-2

RED LAKE AREADflTE i WINTER 1996 REF i 9602

SCALE = 1 : 2400JVX LTD-

13C|OH t IZqOH t liqOH , 90H 60pH , 50pH , 40pH | 30pM OE 20pE , 30pE

TflU TflUNil

N:2

N:3

N:4

N:5

N:6

.0 . 48.0.......O .0 .0 -O

N:2

N:3

N:4

N:5

N:6

eopn sopH , sopn aopn , zopu , lopn , OE t iopE , zopE , aopESPECTRflL M

Nil

N:2

N:3

Ni4

N;5

N:6

SPECTRflL M Nil

Nt2

N:3

Nt4

N:5

Ns6

o •st co

LINE : 1200 N


POLE-DIPOLE RRRRY

VDCPTN rOINT

N r 1. 2. 3. 4. ... •H' SPHCINO = 100.0 FEET

FREENEST RESOURCES

MCKENZIE ISLAND-GRID-2

RED LAKE AREADflTE : WINTER 1996 REF : 9602

SCALE = 1 : 2400JVX LTD-

ISqOH | 14(}OM , 13(]CIH , lOqOH | 90pM , BOpH M , 50pH , 40pH t 30pH , 20pN IQpH , OE , 20pE , 30pE , 40pE , SOpE

TflU TflUNil

N:2

Ni3

Nt4

N:5

N:6

.0 .1 .1 ..O.5 .-O . -O .1 .0 .0 ^ .0 .0 .0

.1 .1 .3 ;i.oo -O .3 .0 .0

.0 .5 .0 .1

.3 .1 .1 .3 .0 .1 .1 .3

.0 o -0\ 2rfl—~. 2..3 .1 .1 .5 .1 .3

A \ Vo i..5 -l .1 .5 .1 -3

15CJOH t 1 4CJON 12()OM , llt|OH 90pM t 80pH , 70pH 30pH OE 20pE | 30pE , 40pE BOpE

SPECTRRL M27.9.5

N:2

N:3

N:4

N:5

N:6

19^^X214.5

.7 189.3

SPECTRflL M N ' !

Ns3

N:4

NsS

N:6

Grid 2Plate 4a

LINE : 900 N


POLE-DIPOLE RRRRY

ffl.

VDtfTH POINT

N : 1. 2. 3. 4. ..-

•fl" SPflCINO s 100.0 FEET

FREEWEST RESOURCES

MCKENZIE ISLflND. GRID-2



RESISTIVITY

MX CHG.

Ni2

N:3

N)4

N:5

N:6

Nil

Ni2

Ni3

Ni4

Ni5

Ni6

l SOON | 14I|OH 120( OH , IICJOH | H)(|OH , 90pH , 80pH , 70J1H | 60pU | 50pH | 4DpH , 30pH , 20pN 20pE , 30pE t 40pE | SOpE , 60pE t 70pE

RESISTIVITY

9K

2K 10.6K

l-SJC 2.2K Nil

Ni2

N:3

Ni4

Ni5

N:6

X P-

TC.

40pE , SOpE , 60pE t 70pE

8.2

8.7 6.5

5 "23. (

24.3

22.2 24.3 24^;Q\. 9 ' 1 M .6N 8.0

22.2 22.1 24.3 ZsVjV 10.4 15.3

22.1 22.1 24.5 26^V\ 10.4

21.4 22.1 22.0 25.1 26.3

ft* C HG. Nil

Ni2

Nt3

Ni4

Ni5

Ni6

LINE : 600 N


POLE-DIPOLE flRRHY

N z 1. 2. 3. 4. ... •fi- SPHCINB = 1 00.0 FEET

FREEWEST RESOURCES

MCKENZIE ISLflND, GRID-2



RESISTIVITY

Ni2

N:3

N:4

'N i o

Nt6

MX CHO.Nil

Ni2

N:3

N:4

Ni5

Ni6

11 • SOPH . 4QOH , 300H , 20DH , 10PH OE , 10PEf—— -r 20DE . 300E , 400E . SOQE . 60PE 70PE . 80QE . 90pEi*) r-^ —— —— —— ——

41-0 44.0

81.0 85-0

46.0 57.0 77.0 130.0 3Q5

94.0 122.0 163.0 2\2.

131.0 141.0 160.0 2Q3-*fr"'228.0 2!9.\)"ft43.0 695

199.Q^-*tmr~l239.0 269.0^3J1Z*6 336^8-^441.0

283.0^3*15-4)—a*e^ 348.0 355.o f27lk.o \27___ Vc^

383.0 389.0 393.0^T3lTW) 330.0 328.0

RESISTIVITY 21.OK 1 5.2K 5.SK Nil

•6K 19.SK Ni2

- 1 O

T.c.pH | 60pt4 , SOpH , 40pH 20pJ t 30pE

18.9 23.3 38.1-6 1.6 1.1 .8 .7

1.8 1.7 1.4 1.2 1.0

-^2^0 1.9 1.5 l

2.7 2.6 2T2 —— ~2T

.6 31.0 36.5 37.9

Ni3

N:4

MsS

N:6

900E

MX CHG. 4.5 3.1 Nil

Ni2

Ni3

Ni4

NiS

N:6

LINE : 300 N


POLE-DIPOLE flRRRY

DEPTH POINT

N - l. 2. 3. 4. ..."H" SPflCINO = 1 00.0 FEET



SCflLE = l: 2400JVX LTD-

2.174^0

RESISTIVITY

IICJOH t IPqOH , 90pH | BOpN | 70pH | 60pH | SOpH , 40pH , 30pH | 20pH , IQpH , 0^ i l OpE , 20pE t 30pE 40pE , SOpE , 60pE , 70pE , 80pE t 90pE IQÔE , HOPE | 1200E

MX CHO.

Nil 50-0 46.0 43.0 45.0 47.0 63-0 86.0__9

Ni2 96.0 97.0 95.0 92.0 88.0 113JJ—T4TTO 206,

N:3 165.0 152.0 160.0 164.0 147.0 171.0 204^

N:4

N:5

N:6 489."0\387.0

252 .

2K

RESISTIVIT N:l

N:2

N:3

N:4

N:5

Ni6

rr-1 IP- i

SOpE ( 60pE t 70pE , 800E | 90pE | 10QOE | 11QOE | 12QOE

3 8.5

70pH , 60pH | SOpH , 40pH

9. 1.3 1.4 1.4 1.4 1.5 1.7 1.8

1.9/ 2.4 2.8 /3.1 3.3 3.1 3.4

2.2 2.8 J. l 3-5 3.5 3.6 4/1

MX CHO. Nil

Ni2

Ni3

Ni4

NiS

Ni6Grid 2Plate 5

o 10 co

LINE : 1800 N

INDUCED POLRRIZRTION SURVEY

POLE-DIPOLE flRRRY

ffl.

N r 1. 2. 3. 4. ... "H" SPfltlNO : 100.0 FEET

FREENEST RESOURCESMCKENZIE ISLRND,GRID-2



60pH [ 500H , 40JH , 30pH , H , OE

RESISTIVITY

N:2

N:3

N:4

N:5

Ni6

RESISTIVITY . O 217.0 N:l

9.0

4K

7K

N:2

N:3

N:4

N:5

Nt6

ir-

MX CHG.

N:2

Ni3

N:4

Ni5

N:6

MX CHO- 13-4 Nil

17.8 N:2

-6.7

N:4

N:5

N:6

LINE : 1500 N


POLE-DIPOLE RRRRY

ffl.

DErTH*r01HT

N - 1 . 2. 3. 4. ... •fl" SPflCING = 100.0 FEET

FREENEST RESOURCESMCKENZIE ISLRND*GRID-2

RED LRKE RRERDflTE : WINTER 1996 REF : 9602


80pH 60pH 40DH , 30J3H "H , OE 20pE

RESISTIVITY RESISTIVITY .4K 5.3K Nil

N:2

N:3

N:4

Ns5

N:6

90pH 70pH [ 60pN | SOpH , 40pH , 30pH , 20pH , IPpH , OE | IPpE , 20pE , 30pE

MX CHO.1.6

Nt2

N:3

N:4

N)5

N:6 7.4

MX CHO- 5^7 9.3 Nsl

Ci .6 Ni2

Nt3

N:4

N:5

N:62.1,7 420

LINE : 1200 N


POLE-DIPOLE RRRflY

OEPTH'VfllMT

N r 1. 2. 3. 4. ... "H' SPnCING = 1 00.0 FEET

FREENEST RESOURCESMCKENZIE ISLRND, GRID-2

RED LRKE RRERDRTE : WINTER 1996 REF : 9602

SCRLE ^ 1: 2400JVX LTD.

i t --'?

n , 80pN , 70pH

RESISTIVITY

40pH , 30pH , 20pH , IPpH , OE | IQpE , 20pE { 30pE , 40pE , 50pE , 60pE

^r3 RESISTIVITY

MX CHO.

NM

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

12()OH , llt|OH , IQtjOH , 90pH , BOpH , 70pM , 60pH | 50pt4 , 40pH , 30pH 20gH^, IQpH |, _ OE ^g^,. 20Rf , 3^PE - 4 0P E j 50P E . 60P E""

2-1 1-1 1-4MX

14.1

N:2

N:3

N:4

N:5

N:6

oCO CO

Grid 2Plate 4

LINE : 2400 N

INDUCED POLflRIZRTION SURVEY

POLE-DIPOLE HRRflY

Z?]

N z 1. 2. 3. 4. ... •H" SPRCING r 100.0 FEET


RED LflKE flREflOflTE : WINTER 1996 REF : 9602


TflU

N:2

N:3

N:4

N:5

N:6

SPECTRPL M

N:2

N:3

N:4

N:5

N:6

•O

50.8

44

90pH i 80pH 40pH 30pH Of

.0 .0 .0 .Q .Q .Q .Q

-o . o .o .o .o .o .o_____ -o .o .o .o .o .o .o

•O .0 .0 .0 .0 .0 .0 .0 .0

•O -O .0 .0 .0 .0 .0 .0

• O .0 .0 .0 .0 .Q .Q

TflU • O N:l

N:2

N:3

N:4

N:5

N:6

H . 40pH 20H

.0 17.5 ,-Q - Ql ' u vJI^ r u • 0\^ . 0____.0.

•Ol V .0 -O/ .0 .0 .0

.0 .0 .0 .0 .0

.0 -O .0 .0 .0

.0 .0 .0 .0

' 0 ' 0 294

.0

SPECTRflL M • O N:l

N:2

N:3

N:4

N:5

N:6

LINE : 2100 N


POLE-DIPOLE RRRflY

a.V

DEPTH POINT

N :: 1. 2. 3. 4. ...

•H" SPflCING = 1 00.0 FEET

FREEWEST RESOURCESMCKENZIE ISLflND. GRID-2


SCflLE :: 1: 2400JVX LTD.

TflU

N:2

N:3

N:4

N:5

N:6

SPECTRflL M

N:2

N:3

N:4

N:5

N:6

80pH 40H Of

TflU• O .0 .0 .0 .0 .0 Nsl

.0 o . 0 .0 .0 .3 Ns2

.0 .0 .0 .1 1.0 .0

.0 .0* n .0 .3 .1

•O -0\ .0 .1 .3 .0 \ . 0 \ .0 ".Q .5 Ns3

•O V -O .1 .1 .0 /O .Q\ .0 1.0 N:4

.0 .0 .0 ^/Q .0 \ . 0 N:5

.0 1.0 .0 .0 .0 .Q .Q N:6

Of

35.7

3TN9N 1.0 .Q .0 .o .0

SPECTRHL M

Ns2

N:3

N:4

Ns5

N:6

LINE : 2400 N


POLE-DIPOLE flRRflY

a.OEPTI/POINT

N r 1. 2. 3. 4.. .̂ —. •H" SPflCING r 100.0 FEET



SCflLE = 1: 2400

JVX LTD-

RESISTIVITY

MX CHO.

N:2

N:3

N:4

N:5

N:6

N:2

N:3

N:4

N:5

N:6

1Q[|OU | 90pH | 80pH | 700U | 60pH | 500H | 400H | 30DH | 20pH Of

""^ RESISTIVITY *0 V U46.0, 62-0 79.0 156.0 192.0 198.0 119.0 112.0^ 60-0 59.0 Nsl

^0X^85^0^/108-0 136-0 134.0 19^0—207rfl—22-4-^

f*~~9*^0 126.0 172-P 29L-fl-"j4TTtr-~3J2.0

591.D l 923^HSS3H-X 119TO—*112-0 165-0/247.0 4*B~.Q 465.0

653\

624ttN

70.0 149.0 22.0 350 O

19^.0 30/4.0 /444.0

N:2

N:3

N:4

N:5

N:6

anomaly

-.6 ..O .1 .3 .3 .5

.8 \2 --9 ' .5

2.8

9^3.

MX CHG. Nsl

N:2

N:3

N:4

N:5

Ns6

LINE : 2100 N


POLE-DIPOLE RRRRY

,

DEPTH*POINT

N r 1. 2. 3. 4, .-.

"R" SPRCING = 100.0 FEET



SCflLE - 1 : 2400

JVX LTD-

RESISTIVITY

N:2

N:3

Ns4

N:5

N:6

N:l

N:2

N:3

N:4

Ns5

Ns6

ilQOH . IPqOH . 90PH 80pH . 70pH . SOPH . 50QH 40pU . 30QH . 20PH . IQPH OET——' i ' F ' r—'- -J—'- -J-.-'—— l—.'--r————*#r±) r ^ f Mf,j rRESISTIVITY^ - m

JQfl.zrTlT.Q

W/iî.o

Ns3

N:4

Ns5

N:6

TP- fligOM , lOqOU , 90pH , 80pM | 70pH . 60pH i 50pU | 40pH | 30pU , 20pM , lOpH , OE

"n:'r"~~ " "-' MX CHG.2.3 . 3.4 3,3 2.1 Nsl

Grid 2Plate 3

oCO

o oCD

O O

O O (M

O O O

O O 00

OoCO

o o

o oCNI

UJZ

co(Xen

oo(M

o o

UJ

a oCO

o oGO

UJ

o o o

UJ

o o(M

a a

UJ

o oCO

2400 2400 N

1500 N

1200 N 1200 N

900 N

600 S

900 S

300 N

O

300 S

600 S

900 S

420

52NO4SW0144 2.17420 DOME 380

1800 S 1800 S

o oCO

o o

o oCM

Oo o

o aCD

ooCO

o a

ooCM

UJ

UJ COcr ea

UJ

o oCM

o o

UJ

o oCO

a aCO

UJ

o o o

UJ

o oCM

FREEWEST RESOURCES CANADA INC.MCKENZIE ISLAND PROPERTY - GRID 2

RED LAKE MINES and MINERALS DIVISION______________N.T.S. 52 N/4 ————.^——

RESISTIVITY CONTOURS (11=2)RESISTIVITY CONTOURS : 500 fc 2500 ohm m


WINTER 1996200 400 600

FEETPLOTTED BY

A.S. FEB. 1996

SCALE 1:2400 PLATE 2

JVX ret. no. 9602

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